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Print a simple progress bar while processing the given iterable.
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Description:
def progressbar(iterable, length=23):
"""Print a simple progress bar while processing the given iterable.
Function |progressbar| does print the progress bar when option
`printprogress` is activted:
>>> from hydpy import pub
>>> pub.options.printprogress = True
You can pass an iterable object. Say you want to calculate the the sum
of all integer values from 1 to 100 and print the progress of the
calculation. Using function |range| (which returns a list in Python 2
and an iterator in Python3, but both are fine), one just has to
interpose function |progressbar|:
>>> from hydpy.core.printtools import progressbar
>>> x_sum = 0
>>> for x in progressbar(range(1, 101)):
... x_sum += x
|---------------------|
***********************
>>> x_sum
5050
To prevent possible interim print commands from dismembering the status
bar, they are delayed until the status bar is complete. For intermediate
print outs of each fiftieth calculation, the result looks as follows:
>>> x_sum = 0
>>> for x in progressbar(range(1, 101)):
... x_sum += x
... if not x % 50:
... print(x, x_sum)
|---------------------|
***********************
50 1275
100 5050
The number of characters of the progress bar can be changed:
>>> for i in progressbar(range(100), length=50):
... continue
|------------------------------------------------|
**************************************************
But its maximum number of characters is restricted by the length of the
given iterable:
>>> for i in progressbar(range(10), length=50):
... continue
|--------|
**********
The smallest possible progress bar has two characters:
>>> for i in progressbar(range(2)):
... continue
||
**
For iterables of length one or zero, no progress bar is plottet:
>>> for i in progressbar(range(1)):
... continue
The same is True when the `printprogress` option is inactivated:
>>> pub.options.printprogress = False
>>> for i in progressbar(range(100)):
... continue
""" |
if hydpy.pub.options.printprogress and (len(iterable) > 1):
temp_name = os.path.join(tempfile.gettempdir(),
'HydPy_progressbar_stdout')
temp_stdout = open(temp_name, 'w')
real_stdout = sys.stdout
try:
sys.stdout = temp_stdout
nmbstars = min(len(iterable), length)
nmbcounts = len(iterable)/nmbstars
indentation = ' '*max(_printprogress_indentation, 0)
with PrintStyle(color=36, font=1, file=real_stdout):
print(' %s|%s|\n%s ' % (indentation,
'-'*(nmbstars-2),
indentation),
end='',
file=real_stdout)
counts = 1.
for next_ in iterable:
counts += 1.
if counts >= nmbcounts:
print(end='*', file=real_stdout)
counts -= nmbcounts
yield next_
finally:
try:
temp_stdout.close()
except BaseException:
pass
sys.stdout = real_stdout
print()
with open(temp_name, 'r') as temp_stdout:
sys.stdout.write(temp_stdout.read())
sys.stdout.flush()
else:
for next_ in iterable:
yield next_ |
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Get the types of all current exchange items supposed to change
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Description:
def GET_parameteritemtypes(self) -> None:
"""Get the types of all current exchange items supposed to change
the values of |Parameter| objects.""" |
for item in state.parameteritems:
self._outputs[item.name] = self._get_itemtype(item) |
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Get the types of all current exchange items supposed to change
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Description:
def GET_conditionitemtypes(self) -> None:
"""Get the types of all current exchange items supposed to change
the values of |StateSequence| or |LogSequence| objects.""" |
for item in state.conditionitems:
self._outputs[item.name] = self._get_itemtype(item) |
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Get the types of all current exchange items supposed to return
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Description:
def GET_getitemtypes(self) -> None:
"""Get the types of all current exchange items supposed to return
the values of |Parameter| or |Sequence| objects or the time series
of |IOSequence| objects.""" |
for item in state.getitems:
type_ = self._get_itemtype(item)
for name, _ in item.yield_name2value():
self._outputs[name] = type_ |
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Get the values of all |Variable| objects observed by the
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Description:
def GET_getitemvalues(self) -> None:
"""Get the values of all |Variable| objects observed by the
current |GetItem| objects.
For |GetItem| objects observing time series,
|HydPyServer.GET_getitemvalues| returns only the values within
the current simulation period.
""" |
for item in state.getitems:
for name, value in item.yield_name2value(state.idx1, state.idx2):
self._outputs[name] = value |
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Assign the |StateSequence| or |LogSequence| object values available
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Description:
def GET_load_conditionvalues(self) -> None:
"""Assign the |StateSequence| or |LogSequence| object values available
for the current simulation start point to the current |HydPy| instance.
When the simulation start point is identical with the initialisation
time point and you did not save conditions for it beforehand, the
"original" initial conditions are used (normally those of the
conditions files of the respective *HydPy* project).
""" |
try:
state.hp.conditions = state.conditions[self._id][state.idx1]
except KeyError:
if state.idx1:
self._statuscode = 500
raise RuntimeError(
f'Conditions for ID `{self._id}` and time point '
f'`{hydpy.pub.timegrids.sim.firstdate}` are required, '
f'but have not been calculated so far.')
else:
state.hp.conditions = state.init_conditions |
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Save the |StateSequence| and |LogSequence| object values of the
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Description:
def GET_save_conditionvalues(self) -> None:
"""Save the |StateSequence| and |LogSequence| object values of the
current |HydPy| instance for the current simulation endpoint.""" |
state.conditions[self._id] = state.conditions.get(self._id, {})
state.conditions[self._id][state.idx2] = state.hp.conditions |
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Save the values of those |ChangeItem| objects which are
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Description:
def GET_save_parameteritemvalues(self) -> None:
"""Save the values of those |ChangeItem| objects which are
handling |Parameter| objects.""" |
for item in state.parameteritems:
state.parameteritemvalues[self._id][item.name] = item.value.copy() |
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Save the current simulation period.
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Description:
def GET_save_timegrid(self) -> None:
"""Save the current simulation period.""" |
state.timegrids[self._id] = copy.deepcopy(hydpy.pub.timegrids.sim) |
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Get the previously saved simulation period.
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Description:
def GET_savedtimegrid(self) -> None:
"""Get the previously saved simulation period.""" |
try:
self._write_timegrid(state.timegrids[self._id])
except KeyError:
self._write_timegrid(hydpy.pub.timegrids.init) |
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Return a function usable as a comparison method for class |Variable|.
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Description:
def _compare_variables_function_generator(
method_string, aggregation_func):
"""Return a function usable as a comparison method for class |Variable|.
Pass the specific method (e.g. `__eq__`) and the corresponding
operator (e.g. `==`) as strings. Also pass either |numpy.all| or
|numpy.any| for aggregating multiple boolean values.
""" |
def comparison_function(self, other):
"""Wrapper for comparison functions for class |Variable|."""
if self is other:
return method_string in ('__eq__', '__le__', '__ge__')
method = getattr(self.value, method_string)
try:
if hasattr(type(other), '__hydpy__get_value__'):
other = other.__hydpy__get_value__()
result = method(other)
if result is NotImplemented:
return result
return aggregation_func(result)
except BaseException:
objecttools.augment_excmessage(
f'While trying to compare variable '
f'{objecttools.elementphrase(self)} with object '
f'`{other}` of type `{objecttools.classname(other)}`')
return comparison_function |
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Raises a |RuntimeError| if at least one of the required values
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Description:
def verify(self) -> None:
"""Raises a |RuntimeError| if at least one of the required values
of a |Variable| object is |None| or |numpy.nan|. The descriptor
`mask` defines, which values are considered to be necessary.
Example on a 0-dimensional |Variable|:
>>> from hydpy.core.variabletools import Variable
>>> class Var(Variable):
... NDIM = 0
... TYPE = float
... __hydpy__connect_variable2subgroup__ = None
... initinfo = 0.0, False
>>> var = Var(None)
>>> import numpy
>>> var.shape = ()
>>> var.value = 1.0
>>> var.verify()
>>> var.value = numpy.nan
>>> var.verify()
Traceback (most recent call last):
...
RuntimeError: For variable `var`, 1 required value has not been set yet.
Example on a 2-dimensional |Variable|:
>>> Var.NDIM = 2
>>> var = Var(None)
>>> var.shape = (2, 3)
>>> var.value = numpy.ones((2,3))
>>> var.value[:, 1] = numpy.nan
>>> var.verify()
Traceback (most recent call last):
...
RuntimeError: For variable `var`, 2 required values \
have not been set yet.
>>> Var.mask = var.mask
>>> Var.mask[0, 1] = False
>>> var.verify()
Traceback (most recent call last):
...
RuntimeError: For variable `var`, 1 required value has not been set yet.
>>> Var.mask[1, 1] = False
>>> var.verify()
""" |
nmbnan: int = numpy.sum(numpy.isnan(
numpy.array(self.value)[self.mask]))
if nmbnan:
if nmbnan == 1:
text = 'value has'
else:
text = 'values have'
raise RuntimeError(
f'For variable {objecttools.devicephrase(self)}, '
f'{nmbnan} required {text} not been set yet.') |
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Average the actual values of the |Variable| object.
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Description:
def average_values(self, *args, **kwargs) -> float:
"""Average the actual values of the |Variable| object.
For 0-dimensional |Variable| objects, the result of method
|Variable.average_values| equals |Variable.value|. The
following example shows this for the sloppily defined class
`SoilMoisture`:
>>> from hydpy.core.variabletools import Variable
>>> class SoilMoisture(Variable):
... NDIM = 0
... TYPE = float
... refweigths = None
... availablemasks = None
... __hydpy__connect_variable2subgroup__ = None
... initinfo = None
>>> sm = SoilMoisture(None)
>>> sm.value = 200.0
>>> sm.average_values()
200.0
When the dimensionality of this class is increased to one,
applying method |Variable.average_values| results in the
following error:
>>> SoilMoisture.NDIM = 1
>>> import numpy
>>> SoilMoisture.shape = (3,)
>>> SoilMoisture.value = numpy.array([200.0, 400.0, 500.0])
>>> sm.average_values()
Traceback (most recent call last):
...
AttributeError: While trying to calculate the mean value \
of variable `soilmoisture`, the following error occurred: Variable \
`soilmoisture` does not define any weighting coefficients.
So model developers have to define another (in this case
1-dimensional) |Variable| subclass (usually a |Parameter|
subclass), and make the relevant object available via property
|Variable.refweights|:
>>> class Area(Variable):
... NDIM = 1
... shape = (3,)
... value = numpy.array([1.0, 1.0, 2.0])
... __hydpy__connect_variable2subgroup__ = None
... initinfo = None
>>> area = Area(None)
>>> SoilMoisture.refweights = property(lambda self: area)
>>> sm.average_values()
400.0
In the examples above, all single entries of `values` are relevant,
which is the default case. However, subclasses of |Variable| can
define an alternative mask, allowing to make some entries
irrelevant. Assume for example, that our `SoilMoisture` object
contains three single values, each one associated with a specific
hydrological response unit (hru). To indicate that soil moisture
is undefined for the third unit, (maybe because it is a water area),
we set the third entry of the verification mask to |False|:
>>> from hydpy.core.masktools import DefaultMask
>>> class Soil(DefaultMask):
... @classmethod
... def new(cls, variable, **kwargs):
... return cls.array2mask([True, True, False])
>>> SoilMoisture.mask = Soil()
>>> sm.average_values()
300.0
Alternatively, method |Variable.average_values| accepts additional
masking information as positional or keyword arguments. Therefore,
the corresponding model must implement some alternative masks,
which are provided by property |Variable.availablemasks|.
We mock this property with a new |Masks| object, handling one
mask for flat soils (only the first hru), one mask for deep soils
(only the second hru), and one mask for water areas (only the
third hru):
>>> class FlatSoil(DefaultMask):
... @classmethod
... def new(cls, variable, **kwargs):
... return cls.array2mask([True, False, False])
>>> class DeepSoil(DefaultMask):
... @classmethod
... def new(cls, variable, **kwargs):
... return cls.array2mask([False, True, False])
>>> class Water(DefaultMask):
... @classmethod
... def new(cls, variable, **kwargs):
... return cls.array2mask([False, False, True])
>>> from hydpy.core import masktools
>>> class Masks(masktools.Masks):
... CLASSES = (FlatSoil,
... DeepSoil,
... Water)
>>> SoilMoisture.availablemasks = Masks(None)
One can pass either the mask classes themselves or their names:
>>> sm.average_values(sm.availablemasks.flatsoil)
200.0
>>> sm.average_values('deepsoil')
400.0
Both variants can be combined:
>>> sm.average_values(sm.availablemasks.deepsoil, 'flatsoil')
300.0
The following error happens if the general mask of the variable
does not contain the given masks:
>>> sm.average_values('flatsoil', 'water')
Traceback (most recent call last):
...
ValueError: While trying to calculate the mean value of variable \
`soilmoisture`, the following error occurred: Based on the arguments \
`('flatsoil', 'water')` and `{}` the mask `CustomMask([ True, False, True])` \
has been determined, which is not a submask of `Soil([ True, True, False])`.
Applying masks with custom options is also supported. One can change
the behaviour of the following mask via the argument `complete`:
>>> class AllOrNothing(DefaultMask):
... @classmethod
... def new(cls, variable, complete):
... if complete:
... bools = [True, True, True]
... else:
... bools = [False, False, False]
... return cls.array2mask(bools)
>>> class Masks(Masks):
... CLASSES = (FlatSoil,
... DeepSoil,
... Water,
... AllOrNothing)
>>> SoilMoisture.availablemasks = Masks(None)
Again, one can apply the mask class directly (but note that one
has to pass the relevant variable as the first argument.):
>>> sm.average_values( # doctest: +ELLIPSIS
... sm.availablemasks.allornothing(sm, complete=True))
Traceback (most recent call last):
...
ValueError: While trying to...
Alternatively, one can pass the mask name as a keyword and pack
the mask's options into a |dict| object:
>>> sm.average_values(allornothing={'complete': False})
nan
You can combine all variants explained above:
>>> sm.average_values(
... 'deepsoil', flatsoil={}, allornothing={'complete': False})
300.0
""" |
try:
if not self.NDIM:
return self.value
mask = self.get_submask(*args, **kwargs)
if numpy.any(mask):
weights = self.refweights[mask]
return numpy.sum(weights*self[mask])/numpy.sum(weights)
return numpy.nan
except BaseException:
objecttools.augment_excmessage(
f'While trying to calculate the mean value of variable '
f'{objecttools.devicephrase(self)}') |
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Get a sub-mask of the mask handled by the actual |Variable| object
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Description:
def get_submask(self, *args, **kwargs) -> masktools.CustomMask:
"""Get a sub-mask of the mask handled by the actual |Variable| object
based on the given arguments.
See the documentation on method |Variable.average_values| for
further information.
""" |
if args or kwargs:
masks = self.availablemasks
mask = masktools.CustomMask(numpy.full(self.shape, False))
for arg in args:
mask = mask + self._prepare_mask(arg, masks)
for key, value in kwargs.items():
mask = mask + self._prepare_mask(key, masks, **value)
if mask not in self.mask:
raise ValueError(
f'Based on the arguments `{args}` and `{kwargs}` '
f'the mask `{repr(mask)}` has been determined, '
f'which is not a submask of `{repr(self.mask)}`.')
else:
mask = self.mask
return mask |
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A list with comments for making string representations
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Description:
def commentrepr(self) -> List[str]:
"""A list with comments for making string representations
more informative.
With option |Options.reprcomments| being disabled,
|Variable.commentrepr| is empty.
""" |
if hydpy.pub.options.reprcomments:
return [f'# {line}' for line in
textwrap.wrap(objecttools.description(self), 72)]
return [] |
<SYSTEM_TASK:>
Return the header of a regular or auxiliary parameter control file.
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Description:
def get_controlfileheader(
model: Union[str, 'modeltools.Model'],
parameterstep: timetools.PeriodConstrArg = None,
simulationstep: timetools.PeriodConstrArg = None) -> str:
"""Return the header of a regular or auxiliary parameter control file.
The header contains the default coding information, the import command
for the given model and the actual parameter and simulation step sizes.
The first example shows that, if you pass the model argument as a
string, you have to take care that this string makes sense:
>>> from hydpy.core.parametertools import get_controlfileheader, Parameter
>>> from hydpy import Period, prepare_model, pub, Timegrids, Timegrid
>>> print(get_controlfileheader(model='no model class',
... parameterstep='-1h',
... simulationstep=Period('1h')))
# -*- coding: utf-8 -*-
<BLANKLINE>
from hydpy.models.no model class import *
<BLANKLINE>
simulationstep('1h')
parameterstep('-1h')
<BLANKLINE>
<BLANKLINE>
The second example shows the saver option to pass the proper model
object. It also shows that function |get_controlfileheader| tries
to gain the parameter and simulation step sizes from the global
|Timegrids| object contained in the module |pub| when necessary:
>>> model = prepare_model('lland_v1')
>>> _ = Parameter.parameterstep('1d')
>>> pub.timegrids = '2000.01.01', '2001.01.01', '1h'
>>> print(get_controlfileheader(model=model))
# -*- coding: utf-8 -*-
<BLANKLINE>
from hydpy.models.lland_v1 import *
<BLANKLINE>
simulationstep('1h')
parameterstep('1d')
<BLANKLINE>
<BLANKLINE>
""" |
with Parameter.parameterstep(parameterstep):
if simulationstep is None:
simulationstep = Parameter.simulationstep
else:
simulationstep = timetools.Period(simulationstep)
return (f"# -*- coding: utf-8 -*-\n\n"
f"from hydpy.models.{model} import *\n\n"
f"simulationstep('{simulationstep}')\n"
f"parameterstep('{Parameter.parameterstep}')\n\n") |
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Call method |Parameter.update| of all "secondary" parameters.
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Description:
def update(self) -> None:
"""Call method |Parameter.update| of all "secondary" parameters.
Directly after initialisation, neither the primary (`control`)
parameters nor the secondary (`derived`) parameters of
application model |hstream_v1| are ready for usage:
>>> from hydpy.models.hstream_v1 import *
>>> parameterstep('1d')
>>> simulationstep('1d')
>>> derived
nmbsegments(?)
c1(?)
c3(?)
c2(?)
Trying to update the values of the secondary parameters while the
primary ones are still not defined, raises errors like the following:
>>> model.parameters.update()
Traceback (most recent call last):
...
AttributeError: While trying to update parameter ``nmbsegments` \
of element `?``, the following error occurred: For variable `lag`, \
no value has been defined so far.
With proper values both for parameter |hstream_control.Lag| and
|hstream_control.Damp|, updating the derived parameters succeeds:
>>> lag(0.0)
>>> damp(0.0)
>>> model.parameters.update()
>>> derived
nmbsegments(0)
c1(0.0)
c3(0.0)
c2(1.0)
""" |
for subpars in self.secondary_subpars:
for par in subpars:
try:
par.update()
except BaseException:
objecttools.augment_excmessage(
f'While trying to update parameter '
f'`{objecttools.elementphrase(par)}`') |
<SYSTEM_TASK:>
Write the control parameters to file.
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Description:
def save_controls(self, filepath: Optional[str] = None,
parameterstep: timetools.PeriodConstrArg = None,
simulationstep: timetools.PeriodConstrArg = None,
auxfiler: 'auxfiletools.Auxfiler' = None):
"""Write the control parameters to file.
Usually, a control file consists of a header (see the documentation
on the method |get_controlfileheader|) and the string representations
of the individual |Parameter| objects handled by the `control`
|SubParameters| object.
The main functionality of method |Parameters.save_controls| is
demonstrated in the documentation on the method |HydPy.save_controls|
of class |HydPy|, which one would apply to write the parameter
information of complete *HydPy* projects. However, to call
|Parameters.save_controls| on individual |Parameters| objects
offers the advantage to choose an arbitrary file path, as shown
in the following example:
>>> from hydpy.models.hstream_v1 import *
>>> parameterstep('1d')
>>> simulationstep('1h')
>>> lag(1.0)
>>> damp(0.5)
>>> from hydpy import Open
>>> with Open():
... model.parameters.save_controls('otherdir/otherfile.py')
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
otherdir/otherfile.py
-------------------------------------
# -*- coding: utf-8 -*-
<BLANKLINE>
from hydpy.models.hstream_v1 import *
<BLANKLINE>
simulationstep('1h')
parameterstep('1d')
<BLANKLINE>
lag(1.0)
damp(0.5)
<BLANKLINE>
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Without a given file path and a proper project configuration,
method |Parameters.save_controls| raises the following error:
>>> model.parameters.save_controls()
Traceback (most recent call last):
...
RuntimeError: To save the control parameters of a model to a file, \
its filename must be known. This can be done, by passing a filename to \
function `save_controls` directly. But in complete HydPy applications, \
it is usally assumed to be consistent with the name of the element \
handling the model.
""" |
if self.control:
variable2auxfile = getattr(auxfiler, str(self.model), None)
lines = [get_controlfileheader(
self.model, parameterstep, simulationstep)]
with Parameter.parameterstep(parameterstep):
for par in self.control:
if variable2auxfile:
auxfilename = variable2auxfile.get_filename(par)
if auxfilename:
lines.append(
f"{par.name}(auxfile='{auxfilename}')\n")
continue
lines.append(repr(par) + '\n')
text = ''.join(lines)
if filepath:
with open(filepath, mode='w', encoding='utf-8') as controlfile:
controlfile.write(text)
else:
filename = objecttools.devicename(self)
if filename == '?':
raise RuntimeError(
'To save the control parameters of a model to a file, '
'its filename must be known. This can be done, by '
'passing a filename to function `save_controls` '
'directly. But in complete HydPy applications, it is '
'usally assumed to be consistent with the name of the '
'element handling the model.')
hydpy.pub.controlmanager.save_file(filename, text) |
<SYSTEM_TASK:>
Try to return the parameter values from the auxiliary control file
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Description:
def _get_values_from_auxiliaryfile(self, auxfile):
"""Try to return the parameter values from the auxiliary control file
with the given name.
Things are a little complicated here. To understand this method, you
should first take a look at the |parameterstep| function.
""" |
try:
frame = inspect.currentframe().f_back.f_back
while frame:
namespace = frame.f_locals
try:
subnamespace = {'model': namespace['model'],
'focus': self}
break
except KeyError:
frame = frame.f_back
else:
raise RuntimeError(
'Cannot determine the corresponding model. Use the '
'`auxfile` keyword in usual parameter control files only.')
filetools.ControlManager.read2dict(auxfile, subnamespace)
try:
subself = subnamespace[self.name]
except KeyError:
raise RuntimeError(
f'The selected file does not define value(s) for '
f'parameter {self.name}')
return subself.values
except BaseException:
objecttools.augment_excmessage(
f'While trying to extract information for parameter '
f'`{self.name}` from file `{auxfile}`') |
<SYSTEM_TASK:>
The actual initial value of the given parameter.
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Description:
def initinfo(self) -> Tuple[Union[float, int, bool], bool]:
"""The actual initial value of the given parameter.
Some |Parameter| subclasses define another value for class
attribute `INIT` than |None| to provide a default value.
Let's define a parameter test class and prepare a function for
initialising it and connecting the resulting instance to a
|SubParameters| object:
>>> from hydpy.core.parametertools import Parameter, SubParameters
>>> class Test(Parameter):
... NDIM = 0
... TYPE = float
... TIME = None
... INIT = 2.0
>>> class SubGroup(SubParameters):
... CLASSES = (Test,)
>>> def prepare():
... subpars = SubGroup(None)
... test = Test(subpars)
... test.__hydpy__connect_variable2subgroup__()
... return test
By default, making use of the `INIT` attribute is disabled:
>>> test = prepare()
>>> test
test(?)
Enable it through setting |Options.usedefaultvalues| to |True|:
>>> from hydpy import pub
>>> pub.options.usedefaultvalues = True
>>> test = prepare()
>>> test
test(2.0)
When no `INIT` attribute is defined, enabling
|Options.usedefaultvalues| has no effect, of course:
>>> del Test.INIT
>>> test = prepare()
>>> test
test(?)
For time-dependent parameter values, the `INIT` attribute is assumed
to be related to a |Parameterstep| of one day:
>>> test.parameterstep = '2d'
>>> test.simulationstep = '12h'
>>> Test.INIT = 2.0
>>> Test.TIME = True
>>> test = prepare()
>>> test
test(4.0)
>>> test.value
1.0
""" |
init = self.INIT
if (init is not None) and hydpy.pub.options.usedefaultvalues:
with Parameter.parameterstep('1d'):
return self.apply_timefactor(init), True
return variabletools.TYPE2MISSINGVALUE[self.TYPE], False |
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Factor to adjust a new value of a time-dependent parameter.
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Description:
def get_timefactor(cls) -> float:
"""Factor to adjust a new value of a time-dependent parameter.
For a time-dependent parameter, its effective value depends on the
simulation step size. Method |Parameter.get_timefactor| returns
the fraction between the current simulation step size and the
current parameter step size.
.. testsetup::
>>> from hydpy import pub
>>> del pub.timegrids
>>> from hydpy.core.parametertools import Parameter
>>> Parameter.simulationstep.delete()
Period()
Method |Parameter.get_timefactor| raises the following error
when time information is not available:
>>> from hydpy.core.parametertools import Parameter
>>> Parameter.get_timefactor()
Traceback (most recent call last):
...
RuntimeError: To calculate the conversion factor for adapting the \
values of the time-dependent parameters, you need to define both a \
parameter and a simulation time step size first.
One can define both time step sizes directly:
>>> _ = Parameter.parameterstep('1d')
>>> _ = Parameter.simulationstep('6h')
>>> Parameter.get_timefactor()
0.25
As usual, the "global" simulation step size of the |Timegrids|
object of module |pub| is prefered:
>>> from hydpy import pub
>>> pub.timegrids = '2000-01-01', '2001-01-01', '12h'
>>> Parameter.get_timefactor()
0.5
""" |
try:
parfactor = hydpy.pub.timegrids.parfactor
except RuntimeError:
if not (cls.parameterstep and cls.simulationstep):
raise RuntimeError(
f'To calculate the conversion factor for adapting '
f'the values of the time-dependent parameters, '
f'you need to define both a parameter and a simulation '
f'time step size first.')
else:
date1 = timetools.Date('2000.01.01')
date2 = date1 + cls.simulationstep
parfactor = timetools.Timegrids(timetools.Timegrid(
date1, date2, cls.simulationstep)).parfactor
return parfactor(cls.parameterstep) |
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The inverse version of method |Parameter.apply_timefactor|.
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Description:
def revert_timefactor(cls, values):
"""The inverse version of method |Parameter.apply_timefactor|.
See the explanations on method Parameter.apply_timefactor| to
understand the following examples:
.. testsetup::
>>> from hydpy import pub
>>> del pub.timegrids
>>> from hydpy.core.parametertools import Parameter
>>> class Par(Parameter):
... TIME = None
>>> Par.parameterstep = '1d'
>>> Par.simulationstep = '6h'
>>> Par.revert_timefactor(4.0)
4.0
>>> Par.TIME = True
>>> Par.revert_timefactor(4.0)
16.0
>>> Par.TIME = False
>>> Par.revert_timefactor(4.0)
1.0
""" |
if cls.TIME is True:
return values / cls.get_timefactor()
if cls.TIME is False:
return values * cls.get_timefactor()
return values |
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Try to find a compressed parameter value representation and
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Description:
def compress_repr(self) -> Optional[str]:
"""Try to find a compressed parameter value representation and
return it.
|Parameter.compress_repr| raises a |NotImplementedError| when
failing to find a compressed representation.
.. testsetup::
>>> from hydpy import pub
>>> del pub.timegrids
For the following examples, we define a 1-dimensional sequence
handling time-dependent floating point values:
>>> from hydpy.core.parametertools import Parameter
>>> class Test(Parameter):
... NDIM = 1
... TYPE = float
... TIME = True
>>> test = Test(None)
Before and directly after defining the parameter shape, `nan`
is returned:
>>> test.compress_repr()
'?'
>>> test
test(?)
>>> test.shape = 4
>>> test
test(?)
Due to the time-dependence of the values of our test class,
we need to specify a parameter and a simulation time step:
>>> test.parameterstep = '1d'
>>> test.simulationstep = '8h'
Compression succeeds when all required values are identical:
>>> test(3.0, 3.0, 3.0, 3.0)
>>> test.values
array([ 1., 1., 1., 1.])
>>> test.compress_repr()
'3.0'
>>> test
test(3.0)
Method |Parameter.compress_repr| returns |None| in case the
required values are not identical:
>>> test(1.0, 2.0, 3.0, 3.0)
>>> test.compress_repr()
>>> test
test(1.0, 2.0, 3.0, 3.0)
If some values are not required, indicate this by the `mask`
descriptor:
>>> import numpy
>>> test(3.0, 3.0, 3.0, numpy.nan)
>>> test
test(3.0, 3.0, 3.0, nan)
>>> Test.mask = numpy.array([True, True, True, False])
>>> test
test(3.0)
For a shape of zero, the string representing includes an empty list:
>>> test.shape = 0
>>> test.compress_repr()
'[]'
>>> test
test([])
Method |Parameter.compress_repr| works similarly for different
|Parameter| subclasses. The following examples focus on a
2-dimensional parameter handling integer values:
>>> from hydpy.core.parametertools import Parameter
>>> class Test(Parameter):
... NDIM = 2
... TYPE = int
... TIME = None
>>> test = Test(None)
>>> test.compress_repr()
'?'
>>> test
test(?)
>>> test.shape = (2, 3)
>>> test
test(?)
>>> test([[3, 3, 3],
... [3, 3, 3]])
>>> test
test(3)
>>> test([[3, 3, -999999],
... [3, 3, 3]])
>>> test
test([[3, 3, -999999],
[3, 3, 3]])
>>> Test.mask = numpy.array([
... [True, True, False],
... [True, True, True]])
>>> test
test(3)
>>> test.shape = (0, 0)
>>> test
test([[]])
""" |
if not hasattr(self, 'value'):
return '?'
if not self:
return f"{self.NDIM * '['}{self.NDIM * ']'}"
unique = numpy.unique(self[self.mask])
if sum(numpy.isnan(unique)) == len(unique.flatten()):
unique = numpy.array([numpy.nan])
else:
unique = self.revert_timefactor(unique)
if len(unique) == 1:
return objecttools.repr_(unique[0])
return None |
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Update the actual simulation values based on the toy-value pairs.
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Description:
def refresh(self) -> None:
"""Update the actual simulation values based on the toy-value pairs.
Usually, one does not need to call refresh explicitly. The
"magic" methods __call__, __setattr__, and __delattr__ invoke
it automatically, when required.
Instantiate a 1-dimensional |SeasonalParameter| object:
>>> from hydpy.core.parametertools import SeasonalParameter
>>> class Par(SeasonalParameter):
... NDIM = 1
... TYPE = float
... TIME = None
>>> par = Par(None)
>>> par.simulationstep = '1d'
>>> par.shape = (None,)
When a |SeasonalParameter| object does not contain any toy-value
pairs yet, the method |SeasonalParameter.refresh| sets all actual
simulation values to zero:
>>> par.values = 1.
>>> par.refresh()
>>> par.values[0]
0.0
When there is only one toy-value pair, its values are relevant
for all actual simulation values:
>>> par.toy_1 = 2. # calls refresh automatically
>>> par.values[0]
2.0
Method |SeasonalParameter.refresh| performs a linear interpolation
for the central time points of each simulation time step. Hence,
in the following example, the original values of the toy-value
pairs do not show up:
>>> par.toy_12_31 = 4.
>>> from hydpy import round_
>>> round_(par.values[0])
2.00274
>>> round_(par.values[-2])
3.99726
>>> par.values[-1]
3.0
If one wants to preserve the original values in this example, one
would have to set the corresponding toy instances in the middle of
some simulation step intervals:
>>> del par.toy_1
>>> del par.toy_12_31
>>> par.toy_1_1_12 = 2
>>> par.toy_12_31_12 = 4.
>>> par.values[0]
2.0
>>> round_(par.values[1])
2.005479
>>> round_(par.values[-2])
3.994521
>>> par.values[-1]
4.0
""" |
if not self:
self.values[:] = 0.
elif len(self) == 1:
values = list(self._toy2values.values())[0]
self.values[:] = self.apply_timefactor(values)
else:
for idx, date in enumerate(
timetools.TOY.centred_timegrid(self.simulationstep)):
values = self.interp(date)
self.values[idx] = self.apply_timefactor(values) |
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Perform a linear value interpolation for the given `date` and
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Description:
def interp(self, date: timetools.Date) -> float:
"""Perform a linear value interpolation for the given `date` and
return the result.
Instantiate a 1-dimensional |SeasonalParameter| object:
>>> from hydpy.core.parametertools import SeasonalParameter
>>> class Par(SeasonalParameter):
... NDIM = 1
... TYPE = float
... TIME = None
>>> par = Par(None)
>>> par.simulationstep = '1d'
>>> par.shape = (None,)
Define three toy-value pairs:
>>> par(_1=2.0, _2=5.0, _12_31=4.0)
Passing a |Date| object matching a |TOY| object exactly returns
the corresponding |float| value:
>>> from hydpy import Date
>>> par.interp(Date('2000.01.01'))
2.0
>>> par.interp(Date('2000.02.01'))
5.0
>>> par.interp(Date('2000.12.31'))
4.0
For all intermediate points, |SeasonalParameter.interp| performs
a linear interpolation:
>>> from hydpy import round_
>>> round_(par.interp(Date('2000.01.02')))
2.096774
>>> round_(par.interp(Date('2000.01.31')))
4.903226
>>> round_(par.interp(Date('2000.02.02')))
4.997006
>>> round_(par.interp(Date('2000.12.30')))
4.002994
Linear interpolation is also allowed between the first and the
last pair when they do not capture the endpoints of the year:
>>> par(_1_2=2.0, _12_30=4.0)
>>> round_(par.interp(Date('2000.12.29')))
3.99449
>>> par.interp(Date('2000.12.30'))
4.0
>>> round_(par.interp(Date('2000.12.31')))
3.333333
>>> round_(par.interp(Date('2000.01.01')))
2.666667
>>> par.interp(Date('2000.01.02'))
2.0
>>> round_(par.interp(Date('2000.01.03')))
2.00551
The following example briefly shows interpolation performed for
a 2-dimensional parameter:
>>> Par.NDIM = 2
>>> par = Par(None)
>>> par.shape = (None, 2)
>>> par(_1_1=[1., 2.], _1_3=[-3, 0.])
>>> result = par.interp(Date('2000.01.02'))
>>> round_(result[0])
-1.0
>>> round_(result[1])
1.0
""" |
xnew = timetools.TOY(date)
xys = list(self)
for idx, (x_1, y_1) in enumerate(xys):
if x_1 > xnew:
x_0, y_0 = xys[idx-1]
break
else:
x_0, y_0 = xys[-1]
x_1, y_1 = xys[0]
return y_0+(y_1-y_0)/(x_1-x_0)*(xnew-x_0) |
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A user-defined value to be used instead of the value of class
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Description:
def alternative_initvalue(self) -> Union[bool, int, float]:
"""A user-defined value to be used instead of the value of class
constant `INIT`.
See the main documentation on class |SolverParameter| for more
information.
""" |
if self._alternative_initvalue is None:
raise AttributeError(
f'No alternative initial value for solver parameter '
f'{objecttools.elementphrase(self)} has been defined so far.')
else:
return self._alternative_initvalue |
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Support for custom company premises model
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Description:
def get_premises_model():
"""
Support for custom company premises model
with developer friendly validation.
""" |
try:
app_label, model_name = PREMISES_MODEL.split('.')
except ValueError:
raise ImproperlyConfigured("OPENINGHOURS_PREMISES_MODEL must be of the"
" form 'app_label.model_name'")
premises_model = get_model(app_label=app_label, model_name=model_name)
if premises_model is None:
raise ImproperlyConfigured("OPENINGHOURS_PREMISES_MODEL refers to"
" model '%s' that has not been installed"
% PREMISES_MODEL)
return premises_model |
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Allows to access global request and read a timestamp from query.
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Description:
def get_now():
"""
Allows to access global request and read a timestamp from query.
""" |
if not get_current_request:
return datetime.datetime.now()
request = get_current_request()
if request:
openinghours_now = request.GET.get('openinghours-now')
if openinghours_now:
return datetime.datetime.strptime(openinghours_now, '%Y%m%d%H%M%S')
return datetime.datetime.now() |
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Returns QuerySet of ClosingRules that are currently valid
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Description:
def get_closing_rule_for_now(location):
"""
Returns QuerySet of ClosingRules that are currently valid
""" |
now = get_now()
if location:
return ClosingRules.objects.filter(company=location,
start__lte=now, end__gte=now)
return Company.objects.first().closingrules_set.filter(start__lte=now,
end__gte=now) |
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Is the company currently open? Pass "now" to test with a specific
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Description:
def is_open(location, now=None):
"""
Is the company currently open? Pass "now" to test with a specific
timestamp. Can be used stand-alone or as a helper.
""" |
if now is None:
now = get_now()
if has_closing_rule_for_now(location):
return False
now_time = datetime.time(now.hour, now.minute, now.second)
if location:
ohs = OpeningHours.objects.filter(company=location)
else:
ohs = Company.objects.first().openinghours_set.all()
for oh in ohs:
is_open = False
# start and end is on the same day
if (oh.weekday == now.isoweekday() and
oh.from_hour <= now_time and
now_time <= oh.to_hour):
is_open = oh
# start and end are not on the same day and we test on the start day
if (oh.weekday == now.isoweekday() and
oh.from_hour <= now_time and
((oh.to_hour < oh.from_hour) and
(now_time < datetime.time(23, 59, 59)))):
is_open = oh
# start and end are not on the same day and we test on the end day
if (oh.weekday == (now.isoweekday() - 1) % 7 and
oh.from_hour >= now_time and
oh.to_hour >= now_time and
oh.to_hour < oh.from_hour):
is_open = oh
# print " 'Special' case after midnight", oh
if is_open is not False:
return oh
return False |
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A |numpy| |numpy.ndarray| with equal weights for all segment
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Description:
def refweights(self):
"""A |numpy| |numpy.ndarray| with equal weights for all segment
junctions..
>>> from hydpy.models.hstream import *
>>> parameterstep('1d')
>>> states.qjoints.shape = 5
>>> states.qjoints.refweights
array([ 0.2, 0.2, 0.2, 0.2, 0.2])
""" |
# pylint: disable=unsubscriptable-object
# due to a pylint bug (see https://github.com/PyCQA/pylint/issues/870)
return numpy.full(self.shape, 1./self.shape[0], dtype=float) |
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Add a directory and optionally its path.
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Description:
def add(self, directory, path=None) -> None:
"""Add a directory and optionally its path.""" |
objecttools.valid_variable_identifier(directory)
if path is None:
path = directory
setattr(self, directory, path) |
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Absolute path pointing to the available working directories.
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Description:
def basepath(self) -> str:
"""Absolute path pointing to the available working directories.
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> from hydpy import repr_, TestIO
>>> with TestIO():
... repr_(filemanager.basepath) # doctest: +ELLIPSIS
'...hydpy/tests/iotesting/projectname/basename'
""" |
return os.path.abspath(
os.path.join(self.projectdir, self.BASEDIR)) |
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Names and paths of the available working directories.
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Description:
def availabledirs(self) -> Folder2Path:
"""Names and paths of the available working directories.
Available working directories are those beeing stored in the
base directory of the respective |FileManager| subclass.
Folders with names starting with an underscore are ignored
(use this for directories handling additional data files,
if you like). Zipped directories, which can be unpacked
on the fly, do also count as available directories:
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> import os
>>> from hydpy import repr_, TestIO
>>> TestIO.clear()
>>> with TestIO():
... os.makedirs('projectname/basename/folder1')
... os.makedirs('projectname/basename/folder2')
... open('projectname/basename/folder3.zip', 'w').close()
... os.makedirs('projectname/basename/_folder4')
... open('projectname/basename/folder5.tar', 'w').close()
... filemanager.availabledirs # doctest: +ELLIPSIS
Folder2Path(folder1=.../projectname/basename/folder1,
folder2=.../projectname/basename/folder2,
folder3=.../projectname/basename/folder3.zip)
""" |
directories = Folder2Path()
for directory in os.listdir(self.basepath):
if not directory.startswith('_'):
path = os.path.join(self.basepath, directory)
if os.path.isdir(path):
directories.add(directory, path)
elif directory.endswith('.zip'):
directories.add(directory[:-4], path)
return directories |
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Name of the current working directory containing the relevant files.
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Description:
def currentdir(self) -> str:
"""Name of the current working directory containing the relevant files.
To show most of the functionality of |property|
|FileManager.currentdir| (unpacking zip files on the fly is
explained in the documentation on function
(|FileManager.zip_currentdir|), we first prepare a |FileManager|
object corresponding to the |FileManager.basepath|
`projectname/basename`:
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> import os
>>> from hydpy import repr_, TestIO
>>> TestIO.clear()
>>> with TestIO():
... os.makedirs('projectname/basename')
... repr_(filemanager.basepath) # doctest: +ELLIPSIS
'...hydpy/tests/iotesting/projectname/basename'
At first, the base directory is empty and asking for the
current working directory results in the following error:
>>> with TestIO():
... filemanager.currentdir # doctest: +ELLIPSIS
Traceback (most recent call last):
...
RuntimeError: The current working directory of the FileManager object \
has not been defined manually and cannot be determined automatically: \
`.../projectname/basename` does not contain any available directories.
If only one directory exists, it is considered as the current
working directory automatically:
>>> with TestIO():
... os.mkdir('projectname/basename/dir1')
... filemanager.currentdir
'dir1'
|property| |FileManager.currentdir| memorises the name of the
current working directory, even if another directory is later
added to the base path:
>>> with TestIO():
... os.mkdir('projectname/basename/dir2')
... filemanager.currentdir
'dir1'
Set the value of |FileManager.currentdir| to |None| to let it
forget the memorised directory. After that, asking for the
current working directory now results in another error, as
it is not clear which directory to select:
>>> with TestIO():
... filemanager.currentdir = None
... filemanager.currentdir # doctest: +ELLIPSIS
Traceback (most recent call last):
...
RuntimeError: The current working directory of the FileManager object \
has not been defined manually and cannot be determined automatically: \
`....../projectname/basename` does contain multiple available directories \
(dir1 and dir2).
Setting |FileManager.currentdir| manually solves the problem:
>>> with TestIO():
... filemanager.currentdir = 'dir1'
... filemanager.currentdir
'dir1'
Remove the current working directory `dir1` with the `del` statement:
>>> with TestIO():
... del filemanager.currentdir
... os.path.exists('projectname/basename/dir1')
False
|FileManager| subclasses can define a default directory name.
When many directories exist and none is selected manually, the
default directory is selected automatically. The following
example shows an error message due to multiple directories
without any having the default name:
>>> with TestIO():
... os.mkdir('projectname/basename/dir1')
... filemanager.DEFAULTDIR = 'dir3'
... del filemanager.currentdir
... filemanager.currentdir # doctest: +ELLIPSIS
Traceback (most recent call last):
...
RuntimeError: The current working directory of the FileManager object \
has not been defined manually and cannot be determined automatically: The \
default directory (dir3) is not among the available directories (dir1 and dir2).
We can fix this by adding the required default directory manually:
>>> with TestIO():
... os.mkdir('projectname/basename/dir3')
... filemanager.currentdir
'dir3'
Setting the |FileManager.currentdir| to `dir4` not only overwrites
the default name, but also creates the required folder:
>>> with TestIO():
... filemanager.currentdir = 'dir4'
... filemanager.currentdir
'dir4'
>>> with TestIO():
... sorted(os.listdir('projectname/basename'))
['dir1', 'dir2', 'dir3', 'dir4']
Failed attempts in removing directories result in error messages
like the following one:
>>> import shutil
>>> from unittest.mock import patch
>>> with patch.object(shutil, 'rmtree', side_effect=AttributeError):
... with TestIO():
... del filemanager.currentdir # doctest: +ELLIPSIS
Traceback (most recent call last):
...
AttributeError: While trying to delete the current working directory \
`.../projectname/basename/dir4` of the FileManager object, the following \
error occurred: ...
Then, the current working directory still exists and is remembered
by |FileManager.currentdir|:
>>> with TestIO():
... filemanager.currentdir
'dir4'
>>> with TestIO():
... sorted(os.listdir('projectname/basename'))
['dir1', 'dir2', 'dir3', 'dir4']
""" |
if self._currentdir is None:
directories = self.availabledirs.folders
if len(directories) == 1:
self.currentdir = directories[0]
elif self.DEFAULTDIR in directories:
self.currentdir = self.DEFAULTDIR
else:
prefix = (f'The current working directory of the '
f'{objecttools.classname(self)} object '
f'has not been defined manually and cannot '
f'be determined automatically:')
if not directories:
raise RuntimeError(
f'{prefix} `{objecttools.repr_(self.basepath)}` '
f'does not contain any available directories.')
if self.DEFAULTDIR is None:
raise RuntimeError(
f'{prefix} `{objecttools.repr_(self.basepath)}` '
f'does contain multiple available directories '
f'({objecttools.enumeration(directories)}).')
raise RuntimeError(
f'{prefix} The default directory ({self.DEFAULTDIR}) '
f'is not among the available directories '
f'({objecttools.enumeration(directories)}).')
return self._currentdir |
<SYSTEM_TASK:>
Absolute path of the current working directory.
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<USER_TASK:>
Description:
def currentpath(self) -> str:
"""Absolute path of the current working directory.
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> from hydpy import repr_, TestIO
>>> with TestIO():
... filemanager.currentdir = 'testdir'
... repr_(filemanager.currentpath) # doctest: +ELLIPSIS
'...hydpy/tests/iotesting/projectname/basename/testdir'
""" |
return os.path.join(self.basepath, self.currentdir) |
<SYSTEM_TASK:>
Names of the files contained in the the current working directory.
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<USER_TASK:>
Description:
def filenames(self) -> List[str]:
"""Names of the files contained in the the current working directory.
Files names starting with underscores are ignored:
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> from hydpy import TestIO
>>> with TestIO():
... filemanager.currentdir = 'testdir'
... open('projectname/basename/testdir/file1.txt', 'w').close()
... open('projectname/basename/testdir/file2.npy', 'w').close()
... open('projectname/basename/testdir/_file1.nc', 'w').close()
... filemanager.filenames
['file1.txt', 'file2.npy']
""" |
return sorted(
fn for fn in os.listdir(self.currentpath)
if not fn.startswith('_')) |
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Absolute path names of the files contained in the current
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Description:
def filepaths(self) -> List[str]:
"""Absolute path names of the files contained in the current
working directory.
Files names starting with underscores are ignored:
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> from hydpy import repr_, TestIO
>>> with TestIO():
... filemanager.currentdir = 'testdir'
... open('projectname/basename/testdir/file1.txt', 'w').close()
... open('projectname/basename/testdir/file2.npy', 'w').close()
... open('projectname/basename/testdir/_file1.nc', 'w').close()
... for filepath in filemanager.filepaths:
... repr_(filepath) # doctest: +ELLIPSIS
'...hydpy/tests/iotesting/projectname/basename/testdir/file1.txt'
'...hydpy/tests/iotesting/projectname/basename/testdir/file2.npy'
""" |
path = self.currentpath
return [os.path.join(path, name) for name in self.filenames] |
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Pack the current working directory in a `zip` file.
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Description:
def zip_currentdir(self) -> None:
"""Pack the current working directory in a `zip` file.
|FileManager| subclasses allow for manual packing and automatic
unpacking of working directories. The only supported format is `zip`.
To avoid possible inconsistencies, origin directories and zip
files are removed after packing or unpacking, respectively.
As an example scenario, we prepare a |FileManager| object with
the current working directory `folder` containing the files
`test1.txt` and `text2.txt`:
>>> from hydpy.core.filetools import FileManager
>>> filemanager = FileManager()
>>> filemanager.BASEDIR = 'basename'
>>> filemanager.projectdir = 'projectname'
>>> import os
>>> from hydpy import repr_, TestIO
>>> TestIO.clear()
>>> basepath = 'projectname/basename'
>>> with TestIO():
... os.makedirs(basepath)
... filemanager.currentdir = 'folder'
... open(f'{basepath}/folder/file1.txt', 'w').close()
... open(f'{basepath}/folder/file2.txt', 'w').close()
... filemanager.filenames
['file1.txt', 'file2.txt']
The directories existing under the base path are identical
with the ones returned by property |FileManager.availabledirs|:
>>> with TestIO():
... sorted(os.listdir(basepath))
... filemanager.availabledirs # doctest: +ELLIPSIS
['folder']
Folder2Path(folder=.../projectname/basename/folder)
After packing the current working directory manually, it is
still counted as a available directory:
>>> with TestIO():
... filemanager.zip_currentdir()
... sorted(os.listdir(basepath))
... filemanager.availabledirs # doctest: +ELLIPSIS
['folder.zip']
Folder2Path(folder=.../projectname/basename/folder.zip)
Instead of the complete directory, only the contained files
are packed:
>>> from zipfile import ZipFile
>>> with TestIO():
... with ZipFile('projectname/basename/folder.zip', 'r') as zp:
... sorted(zp.namelist())
['file1.txt', 'file2.txt']
The zip file is unpacked again, as soon as `folder` becomes
the current working directory:
>>> with TestIO():
... filemanager.currentdir = 'folder'
... sorted(os.listdir(basepath))
... filemanager.availabledirs
... filemanager.filenames # doctest: +ELLIPSIS
['folder']
Folder2Path(folder=.../projectname/basename/folder)
['file1.txt', 'file2.txt']
""" |
with zipfile.ZipFile(f'{self.currentpath}.zip', 'w') as zipfile_:
for filepath, filename in zip(self.filepaths, self.filenames):
zipfile_.write(filename=filepath, arcname=filename)
del self.currentdir |
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Read all network files of the current working directory, structure
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Description:
def load_files(self) -> selectiontools.Selections:
"""Read all network files of the current working directory, structure
their contents in a |selectiontools.Selections| object, and return it.
""" |
devicetools.Node.clear_all()
devicetools.Element.clear_all()
selections = selectiontools.Selections()
for (filename, path) in zip(self.filenames, self.filepaths):
# Ensure both `Node` and `Element`start with a `fresh` memory.
devicetools.Node.extract_new()
devicetools.Element.extract_new()
try:
info = runpy.run_path(path)
except BaseException:
objecttools.augment_excmessage(
f'While trying to load the network file `{path}`')
try:
node: devicetools.Node = info['Node']
element: devicetools.Element = info['Element']
selections += selectiontools.Selection(
filename.split('.')[0],
node.extract_new(),
element.extract_new())
except KeyError as exc:
raise RuntimeError(
f'The class {exc.args[0]} cannot be loaded from the '
f'network file `{path}`.')
selections += selectiontools.Selection(
'complete',
info['Node'].query_all(),
info['Element'].query_all())
return selections |
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Save the |Selection| objects contained in the given |Selections|
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Description:
def save_files(self, selections) -> None:
"""Save the |Selection| objects contained in the given |Selections|
instance to separate network files.""" |
try:
currentpath = self.currentpath
selections = selectiontools.Selections(selections)
for selection in selections:
if selection.name == 'complete':
continue
path = os.path.join(currentpath, selection.name+'.py')
selection.save_networkfile(filepath=path)
except BaseException:
objecttools.augment_excmessage(
'While trying to save selections `%s` into network files'
% selections) |
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Save the given text under the given control filename and the
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Description:
def save_file(self, filename, text):
"""Save the given text under the given control filename and the
current path.""" |
if not filename.endswith('.py'):
filename += '.py'
path = os.path.join(self.currentpath, filename)
with open(path, 'w', encoding="utf-8") as file_:
file_.write(text) |
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Read and return the content of the given file.
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Description:
def load_file(self, filename):
"""Read and return the content of the given file.
If the current directory is not defined explicitly, the directory
name is constructed with the actual simulation start date. If
such an directory does not exist, it is created immediately.
""" |
_defaultdir = self.DEFAULTDIR
try:
if not filename.endswith('.py'):
filename += '.py'
try:
self.DEFAULTDIR = (
'init_' + hydpy.pub.timegrids.sim.firstdate.to_string('os'))
except KeyError:
pass
filepath = os.path.join(self.currentpath, filename)
with open(filepath) as file_:
return file_.read()
except BaseException:
objecttools.augment_excmessage(
'While trying to read the conditions file `%s`'
% filename)
finally:
self.DEFAULTDIR = _defaultdir |
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Save the given text under the given condition filename and the
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Description:
def save_file(self, filename, text):
"""Save the given text under the given condition filename and the
current path.
If the current directory is not defined explicitly, the directory
name is constructed with the actual simulation end date. If
such an directory does not exist, it is created immediately.
""" |
_defaultdir = self.DEFAULTDIR
try:
if not filename.endswith('.py'):
filename += '.py'
try:
self.DEFAULTDIR = (
'init_' + hydpy.pub.timegrids.sim.lastdate.to_string('os'))
except AttributeError:
pass
path = os.path.join(self.currentpath, filename)
with open(path, 'w', encoding="utf-8") as file_:
file_.write(text)
except BaseException:
objecttools.augment_excmessage(
'While trying to write the conditions file `%s`'
% filename)
finally:
self.DEFAULTDIR = _defaultdir |
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Load data from an "external" data file an pass it to
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Description:
def load_file(self, sequence):
"""Load data from an "external" data file an pass it to
the given |IOSequence|.""" |
try:
if sequence.filetype_ext == 'npy':
sequence.series = sequence.adjust_series(
*self._load_npy(sequence))
elif sequence.filetype_ext == 'asc':
sequence.series = sequence.adjust_series(
*self._load_asc(sequence))
elif sequence.filetype_ext == 'nc':
self._load_nc(sequence)
except BaseException:
objecttools.augment_excmessage(
'While trying to load the external data of sequence %s'
% objecttools.devicephrase(sequence)) |
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Write the date stored in |IOSequence.series| of the given
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Description:
def save_file(self, sequence, array=None):
"""Write the date stored in |IOSequence.series| of the given
|IOSequence| into an "external" data file. """ |
if array is None:
array = sequence.aggregate_series()
try:
if sequence.filetype_ext == 'nc':
self._save_nc(sequence, array)
else:
filepath = sequence.filepath_ext
if ((array is not None) and
(array.info['type'] != 'unmodified')):
filepath = (f'{filepath[:-4]}_{array.info["type"]}'
f'{filepath[-4:]}')
if not sequence.overwrite_ext and os.path.exists(filepath):
raise OSError(
f'Sequence {objecttools.devicephrase(sequence)} '
f'is not allowed to overwrite the existing file '
f'`{sequence.filepath_ext}`.')
if sequence.filetype_ext == 'npy':
self._save_npy(array, filepath)
elif sequence.filetype_ext == 'asc':
self._save_asc(array, filepath)
except BaseException:
objecttools.augment_excmessage(
'While trying to save the external data of sequence %s'
% objecttools.devicephrase(sequence)) |
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Prepare a new |NetCDFInterface| object for reading data.
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Description:
def open_netcdf_reader(self, flatten=False, isolate=False, timeaxis=1):
"""Prepare a new |NetCDFInterface| object for reading data.""" |
self._netcdf_reader = netcdftools.NetCDFInterface(
flatten=bool(flatten),
isolate=bool(isolate),
timeaxis=int(timeaxis)) |
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Prepare a new |NetCDFInterface| object for writing data.
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Description:
def open_netcdf_writer(self, flatten=False, isolate=False, timeaxis=1):
"""Prepare a new |NetCDFInterface| object for writing data.""" |
self._netcdf_writer = netcdftools.NetCDFInterface(
flatten=bool(flatten),
isolate=bool(isolate),
timeaxis=int(timeaxis)) |
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Adjust the given precipitation values.
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Description:
def calc_nkor_v1(self):
"""Adjust the given precipitation values.
Required control parameters:
|NHRU|
|KG|
Required input sequence:
|Nied|
Calculated flux sequence:
|NKor|
Basic equation:
:math:`NKor = KG \\cdot Nied`
Example:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(3)
>>> kg(0.8, 1.0, 1.2)
>>> inputs.nied = 10.0
>>> model.calc_nkor_v1()
>>> fluxes.nkor
nkor(8.0, 10.0, 12.0)
""" |
con = self.parameters.control.fastaccess
inp = self.sequences.inputs.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
flu.nkor[k] = con.kg[k] * inp.nied |
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Adjust the given air temperature values.
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Description:
def calc_tkor_v1(self):
"""Adjust the given air temperature values.
Required control parameters:
|NHRU|
|KT|
Required input sequence:
|TemL|
Calculated flux sequence:
|TKor|
Basic equation:
:math:`TKor = KT + TemL`
Example:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(3)
>>> kt(-2.0, 0.0, 2.0)
>>> inputs.teml(1.)
>>> model.calc_tkor_v1()
>>> fluxes.tkor
tkor(-1.0, 1.0, 3.0)
""" |
con = self.parameters.control.fastaccess
inp = self.sequences.inputs.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
flu.tkor[k] = con.kt[k] + inp.teml |
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Calculate reference evapotranspiration after Turc-Wendling.
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Description:
def calc_et0_v1(self):
"""Calculate reference evapotranspiration after Turc-Wendling.
Required control parameters:
|NHRU|
|KE|
|KF|
|HNN|
Required input sequence:
|Glob|
Required flux sequence:
|TKor|
Calculated flux sequence:
|ET0|
Basic equation:
:math:`ET0 = KE \\cdot
\\frac{(8.64 \\cdot Glob+93 \\cdot KF) \\cdot (TKor+22)}
{165 \\cdot (TKor+123) \\cdot (1 + 0.00019 \\cdot min(HNN, 600))}`
Example:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> nhru(3)
>>> ke(1.1)
>>> kf(0.6)
>>> hnn(200.0, 600.0, 1000.0)
>>> inputs.glob = 200.0
>>> fluxes.tkor = 15.0
>>> model.calc_et0_v1()
>>> fluxes.et0
et0(3.07171, 2.86215, 2.86215)
""" |
con = self.parameters.control.fastaccess
inp = self.sequences.inputs.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
flu.et0[k] = (con.ke[k]*(((8.64*inp.glob+93.*con.kf[k]) *
(flu.tkor[k]+22.)) /
(165.*(flu.tkor[k]+123.) *
(1.+0.00019*min(con.hnn[k], 600.))))) |
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Correct the given reference evapotranspiration and update the
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Description:
def calc_et0_wet0_v1(self):
"""Correct the given reference evapotranspiration and update the
corresponding log sequence.
Required control parameters:
|NHRU|
|KE|
|WfET0|
Required input sequence:
|PET|
Calculated flux sequence:
|ET0|
Updated log sequence:
|WET0|
Basic equations:
:math:`ET0_{new} = WfET0 \\cdot KE \\cdot PET +
(1-WfET0) \\cdot ET0_{alt}`
Example:
Prepare four hydrological response units with different value
combinations of parameters |KE| and |WfET0|:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> nhru(4)
>>> ke(0.8, 1.2, 0.8, 1.2)
>>> wfet0(2.0, 2.0, 0.2, 0.2)
Note that the actual value of time dependend parameter |WfET0|
is reduced due the difference between the given parameter and
simulation time steps:
>>> from hydpy import round_
>>> round_(wfet0.values)
1.0, 1.0, 0.1, 0.1
For the first two hydrological response units, the given |PET|
value is modified by -0.4 mm and +0.4 mm, respectively. For the
other two response units, which weight the "new" evaporation
value with 10 %, |ET0| does deviate from the old value of |WET0|
by -0.04 mm and +0.04 mm only:
>>> inputs.pet = 2.0
>>> logs.wet0 = 2.0
>>> model.calc_et0_wet0_v1()
>>> fluxes.et0
et0(1.6, 2.4, 1.96, 2.04)
>>> logs.wet0
wet0([[1.6, 2.4, 1.96, 2.04]])
""" |
con = self.parameters.control.fastaccess
inp = self.sequences.inputs.fastaccess
flu = self.sequences.fluxes.fastaccess
log = self.sequences.logs.fastaccess
for k in range(con.nhru):
flu.et0[k] = (con.wfet0[k]*con.ke[k]*inp.pet +
(1.-con.wfet0[k])*log.wet0[0, k])
log.wet0[0, k] = flu.et0[k] |
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Calculate land use and month specific values of potential
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Description:
def calc_evpo_v1(self):
"""Calculate land use and month specific values of potential
evapotranspiration.
Required control parameters:
|NHRU|
|Lnk|
|FLn|
Required derived parameter:
|MOY|
Required flux sequence:
|ET0|
Calculated flux sequence:
|EvPo|
Additional requirements:
|Model.idx_sim|
Basic equation:
:math:`EvPo = FLn \\cdot ET0`
Example:
For clarity, this is more of a kind of an integration example.
Parameter |FLn| both depends on time (the actual month) and space
(the actual land use). Firstly, let us define a initialization
time period spanning the transition from June to July:
>>> from hydpy import pub
>>> pub.timegrids = '30.06.2000', '02.07.2000', '1d'
Secondly, assume that the considered subbasin is differenciated in
two HRUs, one of primarily consisting of arable land and the other
one of deciduous forests:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(2)
>>> lnk(ACKER, LAUBW)
Thirdly, set the |FLn|
values, one for the relevant months and land use classes:
>>> fln.acker_jun = 1.299
>>> fln.acker_jul = 1.304
>>> fln.laubw_jun = 1.350
>>> fln.laubw_jul = 1.365
Fourthly, the index array connecting the simulation time steps
defined above and the month indexes (0...11) can be retrieved
from the |pub| module. This can be done manually more
conveniently via its update method:
>>> derived.moy.update()
>>> derived.moy
moy(5, 6)
Finally, the actual method (with its simple equation) is applied
as usual:
>>> fluxes.et0 = 2.0
>>> model.idx_sim = 0
>>> model.calc_evpo_v1()
>>> fluxes.evpo
evpo(2.598, 2.7)
>>> model.idx_sim = 1
>>> model.calc_evpo_v1()
>>> fluxes.evpo
evpo(2.608, 2.73)
Reset module |pub| to not interfere the following examples:
>>> del pub.timegrids
""" |
con = self.parameters.control.fastaccess
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
flu.evpo[k] = con.fln[con.lnk[k]-1, der.moy[self.idx_sim]] * flu.et0[k] |
<SYSTEM_TASK:>
Calculate stand precipitation and update the interception storage
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Description:
def calc_nbes_inzp_v1(self):
"""Calculate stand precipitation and update the interception storage
accordingly.
Required control parameters:
|NHRU|
|Lnk|
Required derived parameter:
|KInz|
Required flux sequence:
|NKor|
Calculated flux sequence:
|NBes|
Updated state sequence:
|Inzp|
Additional requirements:
|Model.idx_sim|
Basic equation:
:math:`NBes = \\Bigl \\lbrace
{
{PKor \\ | \\ Inzp = KInz}
\\atop
{0 \\ | \\ Inzp < KInz}
}`
Examples:
Initialize five HRUs with different land usages:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(5)
>>> lnk(SIED_D, FEUCHT, GLETS, FLUSS, SEE)
Define |KInz| values for July the selected land usages directly:
>>> derived.kinz.sied_d_jul = 2.0
>>> derived.kinz.feucht_jul = 1.0
>>> derived.kinz.glets_jul = 0.0
>>> derived.kinz.fluss_jul = 1.0
>>> derived.kinz.see_jul = 1.0
Now we prepare a |MOY| object, that assumes that the first, second,
and third simulation time steps are in June, July, and August
respectively (we make use of the value defined above for July, but
setting the values of parameter |MOY| this way allows for a more
rigorous testing of proper indexing):
>>> derived.moy.shape = 3
>>> derived.moy = 5, 6, 7
>>> model.idx_sim = 1
The dense settlement (|SIED_D|), the wetland area (|FEUCHT|), and
both water areas (|FLUSS| and |SEE|) start with a initial interception
storage of 1/2 mm, the glacier (|GLETS|) and water areas (|FLUSS| and
|SEE|) start with 0 mm. In the first example, actual precipition
is 1 mm:
>>> states.inzp = 0.5, 0.5, 0.0, 1.0, 1.0
>>> fluxes.nkor = 1.0
>>> model.calc_nbes_inzp_v1()
>>> states.inzp
inzp(1.5, 1.0, 0.0, 0.0, 0.0)
>>> fluxes.nbes
nbes(0.0, 0.5, 1.0, 0.0, 0.0)
Only for the settled area, interception capacity is not exceeded,
meaning no stand precipitation occurs. Note that it is common in
define zero interception capacities for glacier areas, but not
mandatory. Also note that the |KInz|, |Inzp| and |NKor| values
given for both water areas are ignored completely, and |Inzp|
and |NBes| are simply set to zero.
If there is no precipitation, there is of course also no stand
precipitation and interception storage remains unchanged:
>>> states.inzp = 0.5, 0.5, 0.0, 0.0, 0.0
>>> fluxes.nkor = 0.
>>> model.calc_nbes_inzp_v1()
>>> states.inzp
inzp(0.5, 0.5, 0.0, 0.0, 0.0)
>>> fluxes.nbes
nbes(0.0, 0.0, 0.0, 0.0, 0.0)
Interception capacities change discontinuously between consecutive
months. This can result in little stand precipitation events in
periods without precipitation:
>>> states.inzp = 1.0, 0.0, 0.0, 0.0, 0.0
>>> derived.kinz.sied_d_jul = 0.6
>>> fluxes.nkor = 0.0
>>> model.calc_nbes_inzp_v1()
>>> states.inzp
inzp(0.6, 0.0, 0.0, 0.0, 0.0)
>>> fluxes.nbes
nbes(0.4, 0.0, 0.0, 0.0, 0.0)
""" |
con = self.parameters.control.fastaccess
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
for k in range(con.nhru):
if con.lnk[k] in (WASSER, FLUSS, SEE):
flu.nbes[k] = 0.
sta.inzp[k] = 0.
else:
flu.nbes[k] = \
max(flu.nkor[k]+sta.inzp[k] -
der.kinz[con.lnk[k]-1, der.moy[self.idx_sim]], 0.)
sta.inzp[k] += flu.nkor[k]-flu.nbes[k] |
<SYSTEM_TASK:>
Calculate the frozen part of stand precipitation.
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Description:
def calc_sbes_v1(self):
"""Calculate the frozen part of stand precipitation.
Required control parameters:
|NHRU|
|TGr|
|TSp|
Required flux sequences:
|TKor|
|NBes|
Calculated flux sequence:
|SBes|
Examples:
In the first example, the threshold temperature of seven hydrological
response units is 0 °C and the corresponding temperature interval of
mixed precipitation 2 °C:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(7)
>>> tgr(0.0)
>>> tsp(2.0)
The value of |NBes| is zero above 1 °C and equal to the value of
|NBes| below -1 °C. Between these temperature values, |NBes|
decreases linearly:
>>> fluxes.nbes = 4.0
>>> fluxes.tkor = -10.0, -1.0, -0.5, 0.0, 0.5, 1.0, 10.0
>>> model.calc_sbes_v1()
>>> fluxes.sbes
sbes(4.0, 4.0, 3.0, 2.0, 1.0, 0.0, 0.0)
Note the special case of a zero temperature interval. With the
actual temperature being equal to the threshold temperature, the
the value of `sbes` is zero:
>>> tsp(0.)
>>> model.calc_sbes_v1()
>>> fluxes.sbes
sbes(4.0, 4.0, 4.0, 0.0, 0.0, 0.0, 0.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
if flu.nbes[k] <= 0.:
flu.sbes[k] = 0.
elif flu.tkor[k] >= (con.tgr[k]+con.tsp[k]/2.):
flu.sbes[k] = 0.
elif flu.tkor[k] <= (con.tgr[k]-con.tsp[k]/2.):
flu.sbes[k] = flu.nbes[k]
else:
flu.sbes[k] = ((((con.tgr[k]+con.tsp[k]/2.)-flu.tkor[k]) /
con.tsp[k])*flu.nbes[k]) |
<SYSTEM_TASK:>
Calculate the potential snowmelt.
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Description:
def calc_wgtf_v1(self):
"""Calculate the potential snowmelt.
Required control parameters:
|NHRU|
|Lnk|
|GTF|
|TRefT|
|TRefN|
|RSchmelz|
|CPWasser|
Required flux sequence:
|TKor|
Calculated fluxes sequence:
|WGTF|
Basic equation:
:math:`WGTF = max(GTF \\cdot (TKor - TRefT), 0) +
max(\\frac{CPWasser}{RSchmelz} \\cdot (TKor - TRefN), 0)`
Examples:
Initialize seven HRUs with identical degree-day factors and
temperature thresholds, but different combinations of land use
and air temperature:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> nhru(7)
>>> lnk(ACKER, LAUBW, FLUSS, SEE, ACKER, ACKER, ACKER)
>>> gtf(5.0)
>>> treft(0.0)
>>> trefn(1.0)
>>> fluxes.tkor = 2.0, 2.0, 2.0, 2.0, -1.0, 0.0, 1.0
Compared to most other LARSIM parameters, the specific heat capacity
and melt heat capacity of water can be seen as fixed properties:
>>> cpwasser(4.1868)
>>> rschmelz(334.0)
Note that the values of the degree-day factor are only half
as much as the given value, due to the simulation step size
being only half as long as the parameter step size:
>>> gtf
gtf(5.0)
>>> gtf.values
array([ 2.5, 2.5, 2.5, 2.5, 2.5, 2.5, 2.5])
After performing the calculation, one can see that the potential
melting rate is identical for the first two HRUs (|ACKER| and
|LAUBW|). The land use class results in no difference, except for
water areas (third and forth HRU, |FLUSS| and |SEE|), where no
potential melt needs to be calculated. The last three HRUs (again
|ACKER|) show the usual behaviour of the degree day method, when the
actual temperature is below (fourth HRU), equal to (fifth HRU) or
above (sixths zone) the threshold temperature. Additionally, the
first two zones show the influence of the additional energy intake
due to "warm" precipitation. Obviously, this additional term is
quite negligible for common parameterizations, even if lower
values for the separate threshold temperature |TRefT| would be
taken into account:
>>> model.calc_wgtf_v1()
>>> fluxes.wgtf
wgtf(5.012535, 5.012535, 0.0, 0.0, 0.0, 0.0, 2.5)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
for k in range(con.nhru):
if con.lnk[k] in (WASSER, FLUSS, SEE):
flu.wgtf[k] = 0.
else:
flu.wgtf[k] = (
max(con.gtf[k]*(flu.tkor[k]-con.treft[k]), 0) +
max(con.cpwasser/con.rschmelz*(flu.tkor[k]-con.trefn[k]), 0.)) |
<SYSTEM_TASK:>
Calculate the actual amount of water melting within the snow cover.
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Description:
def calc_schm_wats_v1(self):
"""Calculate the actual amount of water melting within the snow cover.
Required control parameters:
|NHRU|
|Lnk|
Required flux sequences:
|SBes|
|WGTF|
Calculated flux sequence:
|Schm|
Updated state sequence:
|WATS|
Basic equations:
:math:`\\frac{dWATS}{dt} = SBes - Schm`
:math:`Schm = \\Bigl \\lbrace
{
{WGTF \\ | \\ WATS > 0}
\\atop
{0 \\ | \\ WATS = 0}
}`
Examples:
Initialize two water (|FLUSS| and |SEE|) and four arable land
(|ACKER|) HRUs. Assume the same values for the initial amount
of frozen water (|WATS|) and the frozen part of stand precipitation
(|SBes|), but different values for potential snowmelt (|WGTF|):
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(6)
>>> lnk(FLUSS, SEE, ACKER, ACKER, ACKER, ACKER)
>>> states.wats = 2.0
>>> fluxes.sbes = 1.0
>>> fluxes.wgtf = 1.0, 1.0, 0.0, 1.0, 3.0, 5.0
>>> model.calc_schm_wats_v1()
>>> states.wats
wats(0.0, 0.0, 3.0, 2.0, 0.0, 0.0)
>>> fluxes.schm
schm(0.0, 0.0, 0.0, 1.0, 3.0, 3.0)
For the water areas, both the frozen amount of water and actual melt
are set to zero. For all other land use classes, actual melt
is either limited by potential melt or the available frozen water,
which is the sum of initial frozen water and the frozen part
of stand precipitation.
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
for k in range(con.nhru):
if con.lnk[k] in (WASSER, FLUSS, SEE):
sta.wats[k] = 0.
flu.schm[k] = 0.
else:
sta.wats[k] += flu.sbes[k]
flu.schm[k] = min(flu.wgtf[k], sta.wats[k])
sta.wats[k] -= flu.schm[k] |
<SYSTEM_TASK:>
Calculate the amount of base flow released from the soil.
<END_TASK>
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Description:
def calc_qbb_v1(self):
"""Calculate the amount of base flow released from the soil.
Required control parameters:
|NHRU|
|Lnk|
|Beta|
|FBeta|
Required derived parameter:
|WB|
|WZ|
Required state sequence:
|BoWa|
Calculated flux sequence:
|QBB|
Basic equations:
:math:`Beta_{eff} = \\Bigl \\lbrace
{
{Beta \\ | \\ BoWa \\leq WZ}
\\atop
{Beta \\cdot (1+(FBeta-1)\\cdot\\frac{BoWa-WZ}{NFk-WZ}) \\|\\ BoWa > WZ}
}`
:math:`QBB = \\Bigl \\lbrace
{
{0 \\ | \\ BoWa \\leq WB}
\\atop
{Beta_{eff} \\cdot (BoWa - WB) \\|\\ BoWa > WB}
}`
Examples:
For water and sealed areas, no base flow is calculated (see the
first three HRUs of type |VERS|, |FLUSS|, and |SEE|). No principal
distinction is made between the remaining land use classes (arable
land |ACKER| has been selected for the last five HRUs arbitrarily):
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> nhru(8)
>>> lnk(FLUSS, SEE, VERS, ACKER, ACKER, ACKER, ACKER, ACKER)
>>> beta(0.04)
>>> fbeta(2.0)
>>> nfk(100.0, 100.0, 100.0, 0.0, 100.0, 100.0, 100.0, 200.0)
>>> derived.wb(10.0)
>>> derived.wz(70.0)
Note the time dependence of parameter |Beta|:
>>> beta
beta(0.04)
>>> beta.values
array([ 0.02, 0.02, 0.02, 0.02, 0.02, 0.02, 0.02, 0.02])
In the first example, the actual soil water content |BoWa| is set
to low values. For values below the threshold |WB|, not percolation
occurs. Above |WB| (but below |WZ|), |QBB| increases linearly by
an amount defined by parameter |Beta|:
>>> states.bowa = 20.0, 20.0, 20.0, 0.0, 0.0, 10.0, 20.0, 20.0
>>> model.calc_qbb_v1()
>>> fluxes.qbb
qbb(0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.2, 0.2)
Note that for the last two HRUs the same amount of
base flow generation is determined, in spite of the fact
that both exhibit different relative soil moistures. It is
common to modify this "pure absolute dependency" to a "mixed
absolute/relative dependency" through defining the values of
parameter |WB| indirectly via parameter |RelWB|.
In the second example, the actual soil water content |BoWa| is set
to high values. For values below threshold |WZ|, the discussion above
remains valid. For values above |WZ|, percolation shows a nonlinear
behaviour when factor |FBeta| is set to values larger than one:
>>> nfk(0.0, 0.0, 0.0, 100.0, 100.0, 100.0, 100.0, 200.0)
>>> states.bowa = 0.0, 0.0, 0.0, 60.0, 70.0, 80.0, 100.0, 200.0
>>> model.calc_qbb_v1()
>>> fluxes.qbb
qbb(0.0, 0.0, 0.0, 1.0, 1.2, 1.866667, 3.6, 7.6)
""" |
con = self.parameters.control.fastaccess
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
for k in range(con.nhru):
if ((con.lnk[k] in (VERS, WASSER, FLUSS, SEE)) or
(sta.bowa[k] <= der.wb[k]) or (con.nfk[k] <= 0.)):
flu.qbb[k] = 0.
elif sta.bowa[k] <= der.wz[k]:
flu.qbb[k] = con.beta[k]*(sta.bowa[k]-der.wb[k])
else:
flu.qbb[k] = (con.beta[k]*(sta.bowa[k]-der.wb[k]) *
(1.+(con.fbeta[k]-1.)*((sta.bowa[k]-der.wz[k]) /
(con.nfk[k]-der.wz[k])))) |
<SYSTEM_TASK:>
Calculate direct runoff released from the soil.
<END_TASK>
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Description:
def calc_qdb_v1(self):
"""Calculate direct runoff released from the soil.
Required control parameters:
|NHRU|
|Lnk|
|NFk|
|BSf|
Required state sequence:
|BoWa|
Required flux sequence:
|WaDa|
Calculated flux sequence:
|QDB|
Basic equations:
:math:`QDB = \\Bigl \\lbrace
{
{max(Exz, 0) \\ | \\ SfA \\leq 0}
\\atop
{max(Exz + NFk \\cdot SfA^{BSf+1}, 0) \\ | \\ SfA > 0}
}`
:math:`SFA = (1 - \\frac{BoWa}{NFk})^\\frac{1}{BSf+1} -
\\frac{WaDa}{(BSf+1) \\cdot NFk}`
:math:`Exz = (BoWa + WaDa) - NFk`
Examples:
For water areas (|FLUSS| and |SEE|), sealed areas (|VERS|), and
areas without any soil storage capacity, all water is completely
routed as direct runoff |QDB| (see the first four HRUs). No
principal distinction is made between the remaining land use
classes (arable land |ACKER| has been selected for the last five
HRUs arbitrarily):
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> nhru(9)
>>> lnk(FLUSS, SEE, VERS, ACKER, ACKER, ACKER, ACKER, ACKER, ACKER)
>>> bsf(0.4)
>>> nfk(100.0, 100.0, 100.0, 0.0, 100.0, 100.0, 100.0, 100.0, 100.0)
>>> fluxes.wada = 10.0
>>> states.bowa = (
... 100.0, 100.0, 100.0, 0.0, -0.1, 0.0, 50.0, 100.0, 100.1)
>>> model.calc_qdb_v1()
>>> fluxes.qdb
qdb(10.0, 10.0, 10.0, 10.0, 0.142039, 0.144959, 1.993649, 10.0, 10.1)
With the common |BSf| value of 0.4, the discharge coefficient
increases more or less exponentially with soil moisture.
For soil moisture values slightly below zero or above usable
field capacity, plausible amounts of generated direct runoff
are ensured.
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
aid = self.sequences.aides.fastaccess
for k in range(con.nhru):
if con.lnk[k] == WASSER:
flu.qdb[k] = 0.
elif ((con.lnk[k] in (VERS, FLUSS, SEE)) or
(con.nfk[k] <= 0.)):
flu.qdb[k] = flu.wada[k]
else:
if sta.bowa[k] < con.nfk[k]:
aid.sfa[k] = (
(1.-sta.bowa[k]/con.nfk[k])**(1./(con.bsf[k]+1.)) -
(flu.wada[k]/((con.bsf[k]+1.)*con.nfk[k])))
else:
aid.sfa[k] = 0.
aid.exz[k] = sta.bowa[k]+flu.wada[k]-con.nfk[k]
flu.qdb[k] = aid.exz[k]
if aid.sfa[k] > 0.:
flu.qdb[k] += aid.sfa[k]**(con.bsf[k]+1.)*con.nfk[k]
flu.qdb[k] = max(flu.qdb[k], 0.) |
<SYSTEM_TASK:>
Update soil moisture and correct fluxes if necessary.
<END_TASK>
<USER_TASK:>
Description:
def calc_bowa_v1(self):
"""Update soil moisture and correct fluxes if necessary.
Required control parameters:
|NHRU|
|Lnk|
Required flux sequence:
|WaDa|
Updated state sequence:
|BoWa|
Required (and eventually corrected) flux sequences:
|EvB|
|QBB|
|QIB1|
|QIB2|
|QDB|
Basic equations:
:math:`\\frac{dBoWa}{dt} = WaDa - EvB - QBB - QIB1 - QIB2 - QDB`
:math:`BoWa \\geq 0`
Examples:
For water areas (|FLUSS| and |SEE|) and sealed areas (|VERS|),
soil moisture |BoWa| is simply set to zero and no flux correction
are performed (see the first three HRUs). No principal distinction
is made between the remaining land use classes (arable land |ACKER|
has been selected for the last four HRUs arbitrarily):
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> nhru(7)
>>> lnk(FLUSS, SEE, VERS, ACKER, ACKER, ACKER, ACKER)
>>> states.bowa = 2.0
>>> fluxes.wada = 1.0
>>> fluxes.evb = 1.0, 1.0, 1.0, 0.0, 0.1, 0.2, 0.3
>>> fluxes.qbb = 1.0, 1.0, 1.0, 0.0, 0.2, 0.4, 0.6
>>> fluxes.qib1 = 1.0, 1.0, 1.0, 0.0, 0.3, 0.6, 0.9
>>> fluxes.qib2 = 1.0, 1.0, 1.0, 0.0, 0.4, 0.8, 1.2
>>> fluxes.qdb = 1.0, 1.0, 1.0, 0.0, 0.5, 1.0, 1.5
>>> model.calc_bowa_v1()
>>> states.bowa
bowa(0.0, 0.0, 0.0, 3.0, 1.5, 0.0, 0.0)
>>> fluxes.evb
evb(1.0, 1.0, 1.0, 0.0, 0.1, 0.2, 0.2)
>>> fluxes.qbb
qbb(1.0, 1.0, 1.0, 0.0, 0.2, 0.4, 0.4)
>>> fluxes.qib1
qib1(1.0, 1.0, 1.0, 0.0, 0.3, 0.6, 0.6)
>>> fluxes.qib2
qib2(1.0, 1.0, 1.0, 0.0, 0.4, 0.8, 0.8)
>>> fluxes.qdb
qdb(1.0, 1.0, 1.0, 0.0, 0.5, 1.0, 1.0)
For the seventh HRU, the original total loss terms would result in a
negative soil moisture value. Hence it is reduced to the total loss
term of the sixt HRU, which results exactly in a complete emptying
of the soil storage.
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
aid = self.sequences.aides.fastaccess
for k in range(con.nhru):
if con.lnk[k] in (VERS, WASSER, FLUSS, SEE):
sta.bowa[k] = 0.
else:
aid.bvl[k] = (
flu.evb[k]+flu.qbb[k]+flu.qib1[k]+flu.qib2[k]+flu.qdb[k])
aid.mvl[k] = sta.bowa[k]+flu.wada[k]
if aid.bvl[k] > aid.mvl[k]:
aid.rvl[k] = aid.mvl[k]/aid.bvl[k]
flu.evb[k] *= aid.rvl[k]
flu.qbb[k] *= aid.rvl[k]
flu.qib1[k] *= aid.rvl[k]
flu.qib2[k] *= aid.rvl[k]
flu.qdb[k] *= aid.rvl[k]
sta.bowa[k] = 0.
else:
sta.bowa[k] = aid.mvl[k]-aid.bvl[k] |
<SYSTEM_TASK:>
Aggregate the amount of base flow released by all "soil type" HRUs
<END_TASK>
<USER_TASK:>
Description:
def calc_qbgz_v1(self):
"""Aggregate the amount of base flow released by all "soil type" HRUs
and the "net precipitation" above water areas of type |SEE|.
Water areas of type |SEE| are assumed to be directly connected with
groundwater, but not with the stream network. This is modelled by
adding their (positive or negative) "net input" (|NKor|-|EvI|) to the
"percolation output" of the soil containing HRUs.
Required control parameters:
|Lnk|
|NHRU|
|FHRU|
Required flux sequences:
|QBB|
|NKor|
|EvI|
Calculated state sequence:
|QBGZ|
Basic equation:
:math:`QBGZ = \\Sigma(FHRU \\cdot QBB) +
\\Sigma(FHRU \\cdot (NKor_{SEE}-EvI_{SEE}))`
Examples:
The first example shows that |QBGZ| is the area weighted sum of
|QBB| from "soil type" HRUs like arable land (|ACKER|) and of
|NKor|-|EvI| from water areas of type |SEE|. All other water
areas (|WASSER| and |FLUSS|) and also sealed surfaces (|VERS|)
have no impact on |QBGZ|:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> nhru(6)
>>> lnk(ACKER, ACKER, VERS, WASSER, FLUSS, SEE)
>>> fhru(0.1, 0.2, 0.1, 0.1, 0.1, 0.4)
>>> fluxes.qbb = 2., 4.0, 300.0, 300.0, 300.0, 300.0
>>> fluxes.nkor = 200.0, 200.0, 200.0, 200.0, 200.0, 20.0
>>> fluxes.evi = 100.0, 100.0, 100.0, 100.0, 100.0, 10.0
>>> model.calc_qbgz_v1()
>>> states.qbgz
qbgz(5.0)
The second example shows that large evaporation values above a
HRU of type |SEE| can result in negative values of |QBGZ|:
>>> fluxes.evi[5] = 30
>>> model.calc_qbgz_v1()
>>> states.qbgz
qbgz(-3.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
sta.qbgz = 0.
for k in range(con.nhru):
if con.lnk[k] == SEE:
sta.qbgz += con.fhru[k]*(flu.nkor[k]-flu.evi[k])
elif con.lnk[k] not in (WASSER, FLUSS, VERS):
sta.qbgz += con.fhru[k]*flu.qbb[k] |
<SYSTEM_TASK:>
Aggregate the amount of the first interflow component released
<END_TASK>
<USER_TASK:>
Description:
def calc_qigz1_v1(self):
"""Aggregate the amount of the first interflow component released
by all HRUs.
Required control parameters:
|NHRU|
|FHRU|
Required flux sequence:
|QIB1|
Calculated state sequence:
|QIGZ1|
Basic equation:
:math:`QIGZ1 = \\Sigma(FHRU \\cdot QIB1)`
Example:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> nhru(2)
>>> fhru(0.75, 0.25)
>>> fluxes.qib1 = 1.0, 5.0
>>> model.calc_qigz1_v1()
>>> states.qigz1
qigz1(2.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
sta.qigz1 = 0.
for k in range(con.nhru):
sta.qigz1 += con.fhru[k]*flu.qib1[k] |
<SYSTEM_TASK:>
Aggregate the amount of the second interflow component released
<END_TASK>
<USER_TASK:>
Description:
def calc_qigz2_v1(self):
"""Aggregate the amount of the second interflow component released
by all HRUs.
Required control parameters:
|NHRU|
|FHRU|
Required flux sequence:
|QIB2|
Calculated state sequence:
|QIGZ2|
Basic equation:
:math:`QIGZ2 = \\Sigma(FHRU \\cdot QIB2)`
Example:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> nhru(2)
>>> fhru(0.75, 0.25)
>>> fluxes.qib2 = 1.0, 5.0
>>> model.calc_qigz2_v1()
>>> states.qigz2
qigz2(2.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
sta.qigz2 = 0.
for k in range(con.nhru):
sta.qigz2 += con.fhru[k]*flu.qib2[k] |
<SYSTEM_TASK:>
Aggregate the amount of total direct flow released by all HRUs.
<END_TASK>
<USER_TASK:>
Description:
def calc_qdgz_v1(self):
"""Aggregate the amount of total direct flow released by all HRUs.
Required control parameters:
|Lnk|
|NHRU|
|FHRU|
Required flux sequence:
|QDB|
|NKor|
|EvI|
Calculated flux sequence:
|QDGZ|
Basic equation:
:math:`QDGZ = \\Sigma(FHRU \\cdot QDB) +
\\Sigma(FHRU \\cdot (NKor_{FLUSS}-EvI_{FLUSS}))`
Examples:
The first example shows that |QDGZ| is the area weighted sum of
|QDB| from "land type" HRUs like arable land (|ACKER|) and sealed
surfaces (|VERS|) as well as of |NKor|-|EvI| from water areas of
type |FLUSS|. Water areas of type |WASSER| and |SEE| have no
impact on |QDGZ|:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> nhru(5)
>>> lnk(ACKER, VERS, WASSER, SEE, FLUSS)
>>> fhru(0.1, 0.2, 0.1, 0.2, 0.4)
>>> fluxes.qdb = 2., 4.0, 300.0, 300.0, 300.0
>>> fluxes.nkor = 200.0, 200.0, 200.0, 200.0, 20.0
>>> fluxes.evi = 100.0, 100.0, 100.0, 100.0, 10.0
>>> model.calc_qdgz_v1()
>>> fluxes.qdgz
qdgz(5.0)
The second example shows that large evaporation values above a
HRU of type |FLUSS| can result in negative values of |QDGZ|:
>>> fluxes.evi[4] = 30
>>> model.calc_qdgz_v1()
>>> fluxes.qdgz
qdgz(-3.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
flu.qdgz = 0.
for k in range(con.nhru):
if con.lnk[k] == FLUSS:
flu.qdgz += con.fhru[k]*(flu.nkor[k]-flu.evi[k])
elif con.lnk[k] not in (WASSER, SEE):
flu.qdgz += con.fhru[k]*flu.qdb[k] |
<SYSTEM_TASK:>
Seperate total direct flow into a small and a fast component.
<END_TASK>
<USER_TASK:>
Description:
def calc_qdgz1_qdgz2_v1(self):
"""Seperate total direct flow into a small and a fast component.
Required control parameters:
|A1|
|A2|
Required flux sequence:
|QDGZ|
Calculated state sequences:
|QDGZ1|
|QDGZ2|
Basic equation:
:math:`QDGZ2 = \\frac{(QDGZ-A2)^2}{QDGZ+A1-A2}`
:math:`QDGZ1 = QDGZ - QDGZ1`
Examples:
The formula for calculating the amount of the fast component of
direct flow is borrowed from the famous curve number approach.
Parameter |A2| would be the initial loss and parameter |A1| the
maximum storage, but one should not take this analogy too serious.
Instead, with the value of parameter |A1| set to zero, parameter
|A2| just defines the maximum amount of "slow" direct runoff per
time step:
>>> from hydpy.models.lland import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> a1(0.0)
Let us set the value of |A2| to 4 mm/d, which is 2 mm/12h with
respect to the selected simulation step size:
>>> a2(4.0)
>>> a2
a2(4.0)
>>> a2.value
2.0
Define a test function and let it calculate |QDGZ1| and |QDGZ1| for
values of |QDGZ| ranging from -10 to 100 mm/12h:
>>> from hydpy import UnitTest
>>> test = UnitTest(model,
... model.calc_qdgz1_qdgz2_v1,
... last_example=6,
... parseqs=(fluxes.qdgz,
... states.qdgz1,
... states.qdgz2))
>>> test.nexts.qdgz = -10.0, 0.0, 1.0, 2.0, 3.0, 100.0
>>> test()
| ex. | qdgz | qdgz1 | qdgz2 |
-------------------------------
| 1 | -10.0 | -10.0 | 0.0 |
| 2 | 0.0 | 0.0 | 0.0 |
| 3 | 1.0 | 1.0 | 0.0 |
| 4 | 2.0 | 2.0 | 0.0 |
| 5 | 3.0 | 2.0 | 1.0 |
| 6 | 100.0 | 2.0 | 98.0 |
Setting |A2| to zero and |A1| to 4 mm/d (or 2 mm/12h) results in
a smoother transition:
>>> a2(0.0)
>>> a1(4.0)
>>> test()
| ex. | qdgz | qdgz1 | qdgz2 |
--------------------------------------
| 1 | -10.0 | -10.0 | 0.0 |
| 2 | 0.0 | 0.0 | 0.0 |
| 3 | 1.0 | 0.666667 | 0.333333 |
| 4 | 2.0 | 1.0 | 1.0 |
| 5 | 3.0 | 1.2 | 1.8 |
| 6 | 100.0 | 1.960784 | 98.039216 |
Alternatively, one can mix these two configurations by setting
the values of both parameters to 2 mm/h:
>>> a2(2.0)
>>> a1(2.0)
>>> test()
| ex. | qdgz | qdgz1 | qdgz2 |
-------------------------------------
| 1 | -10.0 | -10.0 | 0.0 |
| 2 | 0.0 | 0.0 | 0.0 |
| 3 | 1.0 | 1.0 | 0.0 |
| 4 | 2.0 | 1.5 | 0.5 |
| 5 | 3.0 | 1.666667 | 1.333333 |
| 6 | 100.0 | 1.99 | 98.01 |
Note the similarity of the results for very high values of total
direct flow |QDGZ| in all three examples, which converge to the sum
of the values of parameter |A1| and |A2|, representing the maximum
value of `slow` direct flow generation per simulation step
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
if flu.qdgz > con.a2:
sta.qdgz2 = (flu.qdgz-con.a2)**2/(flu.qdgz+con.a1-con.a2)
sta.qdgz1 = flu.qdgz-sta.qdgz2
else:
sta.qdgz2 = 0.
sta.qdgz1 = flu.qdgz |
<SYSTEM_TASK:>
Perform the runoff concentration calculation for base flow.
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<USER_TASK:>
Description:
def calc_qbga_v1(self):
"""Perform the runoff concentration calculation for base flow.
The working equation is the analytical solution of the linear storage
equation under the assumption of constant change in inflow during
the simulation time step.
Required derived parameter:
|KB|
Required flux sequence:
|QBGZ|
Calculated state sequence:
|QBGA|
Basic equation:
:math:`QBGA_{neu} = QBGA_{alt} +
(QBGZ_{alt}-QBGA_{alt}) \\cdot (1-exp(-KB^{-1})) +
(QBGZ_{neu}-QBGZ_{alt}) \\cdot (1-KB\\cdot(1-exp(-KB^{-1})))`
Examples:
A normal test case:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> derived.kb(0.1)
>>> states.qbgz.old = 2.0
>>> states.qbgz.new = 4.0
>>> states.qbga.old = 3.0
>>> model.calc_qbga_v1()
>>> states.qbga
qbga(3.800054)
First extreme test case (zero division is circumvented):
>>> derived.kb(0.0)
>>> model.calc_qbga_v1()
>>> states.qbga
qbga(4.0)
Second extreme test case (numerical overflow is circumvented):
>>> derived.kb(1e500)
>>> model.calc_qbga_v1()
>>> states.qbga
qbga(5.0)
""" |
der = self.parameters.derived.fastaccess
old = self.sequences.states.fastaccess_old
new = self.sequences.states.fastaccess_new
if der.kb <= 0.:
new.qbga = new.qbgz
elif der.kb > 1e200:
new.qbga = old.qbga+new.qbgz-old.qbgz
else:
d_temp = (1.-modelutils.exp(-1./der.kb))
new.qbga = (old.qbga +
(old.qbgz-old.qbga)*d_temp +
(new.qbgz-old.qbgz)*(1.-der.kb*d_temp)) |
<SYSTEM_TASK:>
Perform the runoff concentration calculation for the first
<END_TASK>
<USER_TASK:>
Description:
def calc_qiga1_v1(self):
"""Perform the runoff concentration calculation for the first
interflow component.
The working equation is the analytical solution of the linear storage
equation under the assumption of constant change in inflow during
the simulation time step.
Required derived parameter:
|KI1|
Required state sequence:
|QIGZ1|
Calculated state sequence:
|QIGA1|
Basic equation:
:math:`QIGA1_{neu} = QIGA1_{alt} +
(QIGZ1_{alt}-QIGA1_{alt}) \\cdot (1-exp(-KI1^{-1})) +
(QIGZ1_{neu}-QIGZ1_{alt}) \\cdot (1-KI1\\cdot(1-exp(-KI1^{-1})))`
Examples:
A normal test case:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> derived.ki1(0.1)
>>> states.qigz1.old = 2.0
>>> states.qigz1.new = 4.0
>>> states.qiga1.old = 3.0
>>> model.calc_qiga1_v1()
>>> states.qiga1
qiga1(3.800054)
First extreme test case (zero division is circumvented):
>>> derived.ki1(0.0)
>>> model.calc_qiga1_v1()
>>> states.qiga1
qiga1(4.0)
Second extreme test case (numerical overflow is circumvented):
>>> derived.ki1(1e500)
>>> model.calc_qiga1_v1()
>>> states.qiga1
qiga1(5.0)
""" |
der = self.parameters.derived.fastaccess
old = self.sequences.states.fastaccess_old
new = self.sequences.states.fastaccess_new
if der.ki1 <= 0.:
new.qiga1 = new.qigz1
elif der.ki1 > 1e200:
new.qiga1 = old.qiga1+new.qigz1-old.qigz1
else:
d_temp = (1.-modelutils.exp(-1./der.ki1))
new.qiga1 = (old.qiga1 +
(old.qigz1-old.qiga1)*d_temp +
(new.qigz1-old.qigz1)*(1.-der.ki1*d_temp)) |
<SYSTEM_TASK:>
Perform the runoff concentration calculation for the second
<END_TASK>
<USER_TASK:>
Description:
def calc_qiga2_v1(self):
"""Perform the runoff concentration calculation for the second
interflow component.
The working equation is the analytical solution of the linear storage
equation under the assumption of constant change in inflow during
the simulation time step.
Required derived parameter:
|KI2|
Required state sequence:
|QIGZ2|
Calculated state sequence:
|QIGA2|
Basic equation:
:math:`QIGA2_{neu} = QIGA2_{alt} +
(QIGZ2_{alt}-QIGA2_{alt}) \\cdot (1-exp(-KI2^{-1})) +
(QIGZ2_{neu}-QIGZ2_{alt}) \\cdot (1-KI2\\cdot(1-exp(-KI2^{-1})))`
Examples:
A normal test case:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> derived.ki2(0.1)
>>> states.qigz2.old = 2.0
>>> states.qigz2.new = 4.0
>>> states.qiga2.old = 3.0
>>> model.calc_qiga2_v1()
>>> states.qiga2
qiga2(3.800054)
First extreme test case (zero division is circumvented):
>>> derived.ki2(0.0)
>>> model.calc_qiga2_v1()
>>> states.qiga2
qiga2(4.0)
Second extreme test case (numerical overflow is circumvented):
>>> derived.ki2(1e500)
>>> model.calc_qiga2_v1()
>>> states.qiga2
qiga2(5.0)
""" |
der = self.parameters.derived.fastaccess
old = self.sequences.states.fastaccess_old
new = self.sequences.states.fastaccess_new
if der.ki2 <= 0.:
new.qiga2 = new.qigz2
elif der.ki2 > 1e200:
new.qiga2 = old.qiga2+new.qigz2-old.qigz2
else:
d_temp = (1.-modelutils.exp(-1./der.ki2))
new.qiga2 = (old.qiga2 +
(old.qigz2-old.qiga2)*d_temp +
(new.qigz2-old.qigz2)*(1.-der.ki2*d_temp)) |
<SYSTEM_TASK:>
Perform the runoff concentration calculation for "slow" direct runoff.
<END_TASK>
<USER_TASK:>
Description:
def calc_qdga1_v1(self):
"""Perform the runoff concentration calculation for "slow" direct runoff.
The working equation is the analytical solution of the linear storage
equation under the assumption of constant change in inflow during
the simulation time step.
Required derived parameter:
|KD1|
Required state sequence:
|QDGZ1|
Calculated state sequence:
|QDGA1|
Basic equation:
:math:`QDGA1_{neu} = QDGA1_{alt} +
(QDGZ1_{alt}-QDGA1_{alt}) \\cdot (1-exp(-KD1^{-1})) +
(QDGZ1_{neu}-QDGZ1_{alt}) \\cdot (1-KD1\\cdot(1-exp(-KD1^{-1})))`
Examples:
A normal test case:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> derived.kd1(0.1)
>>> states.qdgz1.old = 2.0
>>> states.qdgz1.new = 4.0
>>> states.qdga1.old = 3.0
>>> model.calc_qdga1_v1()
>>> states.qdga1
qdga1(3.800054)
First extreme test case (zero division is circumvented):
>>> derived.kd1(0.0)
>>> model.calc_qdga1_v1()
>>> states.qdga1
qdga1(4.0)
Second extreme test case (numerical overflow is circumvented):
>>> derived.kd1(1e500)
>>> model.calc_qdga1_v1()
>>> states.qdga1
qdga1(5.0)
""" |
der = self.parameters.derived.fastaccess
old = self.sequences.states.fastaccess_old
new = self.sequences.states.fastaccess_new
if der.kd1 <= 0.:
new.qdga1 = new.qdgz1
elif der.kd1 > 1e200:
new.qdga1 = old.qdga1+new.qdgz1-old.qdgz1
else:
d_temp = (1.-modelutils.exp(-1./der.kd1))
new.qdga1 = (old.qdga1 +
(old.qdgz1-old.qdga1)*d_temp +
(new.qdgz1-old.qdgz1)*(1.-der.kd1*d_temp)) |
<SYSTEM_TASK:>
Perform the runoff concentration calculation for "fast" direct runoff.
<END_TASK>
<USER_TASK:>
Description:
def calc_qdga2_v1(self):
"""Perform the runoff concentration calculation for "fast" direct runoff.
The working equation is the analytical solution of the linear storage
equation under the assumption of constant change in inflow during
the simulation time step.
Required derived parameter:
|KD2|
Required state sequence:
|QDGZ2|
Calculated state sequence:
|QDGA2|
Basic equation:
:math:`QDGA2_{neu} = QDGA2_{alt} +
(QDGZ2_{alt}-QDGA2_{alt}) \\cdot (1-exp(-KD2^{-1})) +
(QDGZ2_{neu}-QDGZ2_{alt}) \\cdot (1-KD2\\cdot(1-exp(-KD2^{-1})))`
Examples:
A normal test case:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> derived.kd2(0.1)
>>> states.qdgz2.old = 2.0
>>> states.qdgz2.new = 4.0
>>> states.qdga2.old = 3.0
>>> model.calc_qdga2_v1()
>>> states.qdga2
qdga2(3.800054)
First extreme test case (zero division is circumvented):
>>> derived.kd2(0.0)
>>> model.calc_qdga2_v1()
>>> states.qdga2
qdga2(4.0)
Second extreme test case (numerical overflow is circumvented):
>>> derived.kd2(1e500)
>>> model.calc_qdga2_v1()
>>> states.qdga2
qdga2(5.0)
""" |
der = self.parameters.derived.fastaccess
old = self.sequences.states.fastaccess_old
new = self.sequences.states.fastaccess_new
if der.kd2 <= 0.:
new.qdga2 = new.qdgz2
elif der.kd2 > 1e200:
new.qdga2 = old.qdga2+new.qdgz2-old.qdgz2
else:
d_temp = (1.-modelutils.exp(-1./der.kd2))
new.qdga2 = (old.qdga2 +
(old.qdgz2-old.qdga2)*d_temp +
(new.qdgz2-old.qdgz2)*(1.-der.kd2*d_temp)) |
<SYSTEM_TASK:>
Calculate the final runoff.
<END_TASK>
<USER_TASK:>
Description:
def calc_q_v1(self):
"""Calculate the final runoff.
Note that, in case there are water areas, their |NKor| values are
added and their |EvPo| values are subtracted from the "potential"
runoff value, if possible. This hold true for |WASSER| only and is
due to compatibility with the original LARSIM implementation. Using land
type |WASSER| can result in problematic modifications of simulated
runoff series. It seems advisable to use land type |FLUSS| and/or
land type |SEE| instead.
Required control parameters:
|NHRU|
|FHRU|
|Lnk|
|NegQ|
Required flux sequence:
|NKor|
Updated flux sequence:
|EvI|
Required state sequences:
|QBGA|
|QIGA1|
|QIGA2|
|QDGA1|
|QDGA2|
Calculated flux sequence:
|lland_fluxes.Q|
Basic equations:
:math:`Q = QBGA + QIGA1 + QIGA2 + QDGA1 + QDGA2 +
NKor_{WASSER} - EvI_{WASSER}`
:math:`Q \\geq 0`
Examples:
When there are no water areas in the respective subbasin (we
choose arable land |ACKER| arbitrarily), the different runoff
components are simply summed up:
>>> from hydpy.models.lland import *
>>> parameterstep()
>>> nhru(3)
>>> lnk(ACKER, ACKER, ACKER)
>>> fhru(0.5, 0.2, 0.3)
>>> negq(False)
>>> states.qbga = 0.1
>>> states.qiga1 = 0.3
>>> states.qiga2 = 0.5
>>> states.qdga1 = 0.7
>>> states.qdga2 = 0.9
>>> fluxes.nkor = 10.0
>>> fluxes.evi = 4.0, 5.0, 3.0
>>> model.calc_q_v1()
>>> fluxes.q
q(2.5)
>>> fluxes.evi
evi(4.0, 5.0, 3.0)
The defined values of interception evaporation do not show any
impact on the result of the given example, the predefined values
for sequence |EvI| remain unchanged. But when the first HRU is
assumed to be a water area (|WASSER|), its adjusted precipitaton
|NKor| value and its interception evaporation |EvI| value are added
to and subtracted from |lland_fluxes.Q| respectively:
>>> control.lnk(WASSER, VERS, NADELW)
>>> model.calc_q_v1()
>>> fluxes.q
q(5.5)
>>> fluxes.evi
evi(4.0, 5.0, 3.0)
Note that only 5 mm are added (instead of the |NKor| value 10 mm)
and that only 2 mm are substracted (instead of the |EvI| value 4 mm,
as the first HRU`s area only accounts for 50 % of the subbasin area.
Setting also the land use class of the second HRU to land type
|WASSER| and resetting |NKor| to zero would result in overdrying.
To avoid this, both actual water evaporation values stored in
sequence |EvI| are reduced by the same factor:
>>> control.lnk(WASSER, WASSER, NADELW)
>>> fluxes.nkor = 0.0
>>> model.calc_q_v1()
>>> fluxes.q
q(0.0)
>>> fluxes.evi
evi(3.333333, 4.166667, 3.0)
The handling from water areas of type |FLUSS| and |SEE| differs
from those of type |WASSER|, as these do receive their net input
before the runoff concentration routines are applied. This
should be more realistic in most cases (especially for type |SEE|
representing lakes not direct connected to the stream network).
But it could sometimes result in negative outflow values. This
is avoided by simply setting |lland_fluxes.Q| to zero and adding
the truncated negative outflow value to the |EvI| value of all
HRUs of type |FLUSS| and |SEE|:
>>> control.lnk(FLUSS, SEE, NADELW)
>>> states.qbga = -1.0
>>> states.qdga2 = -1.5
>>> fluxes.evi = 4.0, 5.0, 3.0
>>> model.calc_q_v1()
>>> fluxes.q
q(0.0)
>>> fluxes.evi
evi(2.571429, 3.571429, 3.0)
This adjustment of |EvI| is only correct regarding the total
water balance. Neither spatial nor temporal consistency of the
resulting |EvI| values are assured. In the most extreme case,
even negative |EvI| values might occur. This seems acceptable,
as long as the adjustment of |EvI| is rarely triggered. When in
doubt about this, check sequences |EvPo| and |EvI| of HRUs of
types |FLUSS| and |SEE| for possible discrepancies. Also note
that there might occur unnecessary corrections of |lland_fluxes.Q|
in case landtype |WASSER| is combined with either landtype
|SEE| or |FLUSS|.
Eventually you might want to avoid correcting |lland_fluxes.Q|.
This can be achieved by setting parameter |NegQ| to `True`:
>>> negq(True)
>>> fluxes.evi = 4.0, 5.0, 3.0
>>> model.calc_q_v1()
>>> fluxes.q
q(-1.0)
>>> fluxes.evi
evi(4.0, 5.0, 3.0)
""" |
con = self.parameters.control.fastaccess
flu = self.sequences.fluxes.fastaccess
sta = self.sequences.states.fastaccess
aid = self.sequences.aides.fastaccess
flu.q = sta.qbga+sta.qiga1+sta.qiga2+sta.qdga1+sta.qdga2
if (not con.negq) and (flu.q < 0.):
d_area = 0.
for k in range(con.nhru):
if con.lnk[k] in (FLUSS, SEE):
d_area += con.fhru[k]
if d_area > 0.:
for k in range(con.nhru):
if con.lnk[k] in (FLUSS, SEE):
flu.evi[k] += flu.q/d_area
flu.q = 0.
aid.epw = 0.
for k in range(con.nhru):
if con.lnk[k] == WASSER:
flu.q += con.fhru[k]*flu.nkor[k]
aid.epw += con.fhru[k]*flu.evi[k]
if (flu.q > aid.epw) or con.negq:
flu.q -= aid.epw
elif aid.epw > 0.:
for k in range(con.nhru):
if con.lnk[k] == WASSER:
flu.evi[k] *= flu.q/aid.epw
flu.q = 0. |
<SYSTEM_TASK:>
Performs the actual interpolation or extrapolation.
<END_TASK>
<USER_TASK:>
Description:
def calc_outputs_v1(self):
"""Performs the actual interpolation or extrapolation.
Required control parameters:
|XPoints|
|YPoints|
Required derived parameter:
|NmbPoints|
|NmbBranches|
Required flux sequence:
|Input|
Calculated flux sequence:
|Outputs|
Examples:
As a simple example, assume a weir directing all discharge into
`branch1` until the capacity limit of 2 m³/s is reached. The
discharge exceeding this threshold is directed into `branch2`:
>>> from hydpy.models.hbranch import *
>>> parameterstep()
>>> xpoints(0., 2., 4.)
>>> ypoints(branch1=[0., 2., 2.],
... branch2=[0., 0., 2.])
>>> model.parameters.update()
Low discharge example (linear interpolation between the first two
supporting point pairs):
>>> fluxes.input = 1.
>>> model.calc_outputs_v1()
>>> fluxes.outputs
outputs(branch1=1.0,
branch2=0.0)
Medium discharge example (linear interpolation between the second
two supporting point pairs):
>>> fluxes.input = 3.
>>> model.calc_outputs_v1()
>>> print(fluxes.outputs)
outputs(branch1=2.0,
branch2=1.0)
High discharge example (linear extrapolation beyond the second two
supporting point pairs):
>>> fluxes.input = 5.
>>> model.calc_outputs_v1()
>>> fluxes.outputs
outputs(branch1=2.0,
branch2=3.0)
Non-monotonous relationships and balance violations are allowed,
e.g.:
>>> xpoints(0., 2., 4., 6.)
>>> ypoints(branch1=[0., 2., 0., 0.],
... branch2=[0., 0., 2., 4.])
>>> model.parameters.update()
>>> fluxes.input = 7.
>>> model.calc_outputs_v1()
>>> fluxes.outputs
outputs(branch1=0.0,
branch2=5.0)
""" |
con = self.parameters.control.fastaccess
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
# Search for the index of the two relevant x points...
for pdx in range(1, der.nmbpoints):
if con.xpoints[pdx] > flu.input:
break
# ...and use it for linear interpolation (or extrapolation).
for bdx in range(der.nmbbranches):
flu.outputs[bdx] = (
(flu.input-con.xpoints[pdx-1]) *
(con.ypoints[bdx, pdx]-con.ypoints[bdx, pdx-1]) /
(con.xpoints[pdx]-con.xpoints[pdx-1]) +
con.ypoints[bdx, pdx-1]) |
<SYSTEM_TASK:>
Connect the |LinkSequence| instances handled by the actual model
<END_TASK>
<USER_TASK:>
Description:
def connect(self):
"""Connect the |LinkSequence| instances handled by the actual model
to the |NodeSequence| instances handled by one inlet node and
multiple oulet nodes.
The HydPy-H-Branch model passes multiple output values to different
outlet nodes. This requires additional information regarding the
`direction` of each output value. Therefore, node names are used
as keywords. Assume the discharge values of both nodes `inflow1`
and `inflow2` shall be branched to nodes `outflow1` and `outflow2`
via element `branch`:
>>> from hydpy import *
>>> branch = Element('branch',
... inlets=['inflow1', 'inflow2'],
... outlets=['outflow1', 'outflow2'])
Then parameter |YPoints| relates different supporting points via
its keyword arguments to the respective nodes:
>>> from hydpy.models.hbranch import *
>>> parameterstep()
>>> xpoints(0.0, 3.0)
>>> ypoints(outflow1=[0.0, 1.0], outflow2=[0.0, 2.0])
>>> parameters.update()
After connecting the model with its element the total discharge
value of nodes `inflow1` and `inflow2` can be properly divided:
>>> branch.model = model
>>> branch.inlets.inflow1.sequences.sim = 1.0
>>> branch.inlets.inflow2.sequences.sim = 5.0
>>> model.doit(0)
>>> print(branch.outlets.outflow1.sequences.sim)
sim(2.0)
>>> print(branch.outlets.outflow2.sequences.sim)
sim(4.0)
In case of missing (or misspelled) outlet nodes, the following
error is raised:
>>> branch.outlets.mutable = True
>>> del branch.outlets.outflow1
>>> parameters.update()
>>> model.connect()
Traceback (most recent call last):
...
RuntimeError: Model `hbranch` of element `branch` tried to connect \
to an outlet node named `outflow1`, which is not an available outlet node \
of element `branch`.
""" |
nodes = self.element.inlets
total = self.sequences.inlets.total
if total.shape != (len(nodes),):
total.shape = len(nodes)
for idx, node in enumerate(nodes):
double = node.get_double('inlets')
total.set_pointer(double, idx)
for (idx, name) in enumerate(self.nodenames):
try:
outlet = getattr(self.element.outlets, name)
double = outlet.get_double('outlets')
except AttributeError:
raise RuntimeError(
f'Model {objecttools.elementphrase(self)} tried '
f'to connect to an outlet node named `{name}`, '
f'which is not an available outlet node of element '
f'`{self.element.name}`.')
self.sequences.outlets.branched.set_pointer(double, idx) |
<SYSTEM_TASK:>
Determine the number of response functions.
<END_TASK>
<USER_TASK:>
Description:
def update(self):
"""Determine the number of response functions.
>>> from hydpy.models.arma import *
>>> parameterstep('1d')
>>> responses(((1., 2.), (1.,)), th_3=((1.,), (1., 2., 3.)))
>>> derived.nmb.update()
>>> derived.nmb
nmb(2)
Note that updating parameter `nmb` sets the shape of the flux
sequences |QPIn|, |QPOut|, |QMA|, and |QAR| automatically.
>>> fluxes.qpin
qpin(nan, nan)
>>> fluxes.qpout
qpout(nan, nan)
>>> fluxes.qma
qma(nan, nan)
>>> fluxes.qar
qar(nan, nan)
""" |
pars = self.subpars.pars
responses = pars.control.responses
fluxes = pars.model.sequences.fluxes
self(len(responses))
fluxes.qpin.shape = self.value
fluxes.qpout.shape = self.value
fluxes.qma.shape = self.value
fluxes.qar.shape = self.value |
<SYSTEM_TASK:>
Determine all AR coefficients.
<END_TASK>
<USER_TASK:>
Description:
def update(self):
"""Determine all AR coefficients.
>>> from hydpy.models.arma import *
>>> parameterstep('1d')
>>> responses(((1., 2.), (1.,)), th_3=((1.,), (1., 2., 3.)))
>>> derived.ar_coefs.update()
>>> derived.ar_coefs
ar_coefs([[1.0, 2.0],
[1.0, nan]])
Note that updating parameter `ar_coefs` sets the shape of the log
sequence |LogOut| automatically.
>>> logs.logout
logout([[nan, nan],
[nan, nan]])
""" |
pars = self.subpars.pars
coefs = pars.control.responses.ar_coefs
self.shape = coefs.shape
self(coefs)
pars.model.sequences.logs.logout.shape = self.shape |
<SYSTEM_TASK:>
Determine all MA coefficients.
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Description:
def update(self):
"""Determine all MA coefficients.
>>> from hydpy.models.arma import *
>>> parameterstep('1d')
>>> responses(((1., 2.), (1.,)), th_3=((1.,), (1., 2., 3.)))
>>> derived.ma_coefs.update()
>>> derived.ma_coefs
ma_coefs([[1.0, nan, nan],
[1.0, 2.0, 3.0]])
Note that updating parameter `ar_coefs` sets the shape of the log
sequence |LogIn| automatically.
>>> logs.login
login([[nan, nan, nan],
[nan, nan, nan]])
""" |
pars = self.subpars.pars
coefs = pars.control.responses.ma_coefs
self.shape = coefs.shape
self(coefs)
pars.model.sequences.logs.login.shape = self.shape |
<SYSTEM_TASK:>
Try to convert the given argument to a |list| of |Selection|
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Description:
def __getiterable(value): # ToDo: refactor
"""Try to convert the given argument to a |list| of |Selection|
objects and return it.
""" |
if isinstance(value, Selection):
return [value]
try:
for selection in value:
if not isinstance(selection, Selection):
raise TypeError
return list(value)
except TypeError:
raise TypeError(
f'Binary operations on Selections objects are defined for '
f'other Selections objects, single Selection objects, or '
f'iterables containing `Selection` objects, but the type of '
f'the given argument is `{objecttools.classname(value)}`.') |
<SYSTEM_TASK:>
Return the network upstream of the given starting point, including
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Description:
def search_upstream(self, device: devicetools.Device,
name: str = 'upstream') -> 'Selection':
"""Return the network upstream of the given starting point, including
the starting point itself.
>>> from hydpy.core.examples import prepare_full_example_2
>>> hp, pub, _ = prepare_full_example_2()
You can pass both |Node| and |Element| objects and, optionally,
the name of the newly created |Selection| object:
>>> test = pub.selections.complete.copy('test')
>>> test.search_upstream(hp.nodes.lahn_2)
Selection("upstream",
nodes=("dill", "lahn_1", "lahn_2"),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"stream_dill_lahn_2", "stream_lahn_1_lahn_2"))
>>> test.search_upstream(
... hp.elements.stream_lahn_1_lahn_2, 'UPSTREAM')
Selection("UPSTREAM",
nodes="lahn_1",
elements=("land_lahn_1", "stream_lahn_1_lahn_2"))
Wrong device specifications result in errors like the following:
>>> test.search_upstream(1)
Traceback (most recent call last):
...
TypeError: While trying to determine the upstream network of \
selection `test`, the following error occurred: Either a `Node` or \
an `Element` object is required as the "outlet device", but the given \
`device` value is of type `int`.
>>> pub.selections.headwaters.search_upstream(hp.nodes.lahn_3)
Traceback (most recent call last):
...
KeyError: "While trying to determine the upstream network of \
selection `headwaters`, the following error occurred: 'No node named \
`lahn_3` available.'"
Method |Selection.select_upstream| restricts the current selection
to the one determined with the method |Selection.search_upstream|:
>>> test.select_upstream(hp.nodes.lahn_2)
Selection("test",
nodes=("dill", "lahn_1", "lahn_2"),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"stream_dill_lahn_2", "stream_lahn_1_lahn_2"))
On the contrary, the method |Selection.deselect_upstream| restricts
the current selection to all devices not determined by method
|Selection.search_upstream|:
>>> complete = pub.selections.complete.deselect_upstream(
... hp.nodes.lahn_2)
>>> complete
Selection("complete",
nodes="lahn_3",
elements=("land_lahn_3", "stream_lahn_2_lahn_3"))
If necessary, include the "outlet device" manually afterwards:
>>> complete.nodes += hp.nodes.lahn_2
>>> complete
Selection("complete",
nodes=("lahn_2", "lahn_3"),
elements=("land_lahn_3", "stream_lahn_2_lahn_3"))
""" |
try:
selection = Selection(name)
if isinstance(device, devicetools.Node):
node = self.nodes[device.name]
return self.__get_nextnode(node, selection)
if isinstance(device, devicetools.Element):
element = self.elements[device.name]
return self.__get_nextelement(element, selection)
raise TypeError(
f'Either a `Node` or an `Element` object is required '
f'as the "outlet device", but the given `device` value '
f'is of type `{objecttools.classname(device)}`.')
except BaseException:
objecttools.augment_excmessage(
f'While trying to determine the upstream network of '
f'selection `{self.name}`') |
<SYSTEM_TASK:>
Restrict the current selection to the network upstream of the given
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Description:
def select_upstream(self, device: devicetools.Device) -> 'Selection':
"""Restrict the current selection to the network upstream of the given
starting point, including the starting point itself.
See the documentation on method |Selection.search_upstream| for
additional information.
""" |
upstream = self.search_upstream(device)
self.nodes = upstream.nodes
self.elements = upstream.elements
return self |
<SYSTEM_TASK:>
Return a |Selection| object containing only the elements
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Description:
def search_modeltypes(self, *models: ModelTypesArg,
name: str = 'modeltypes') -> 'Selection':
"""Return a |Selection| object containing only the elements
currently handling models of the given types.
>>> from hydpy.core.examples import prepare_full_example_2
>>> hp, pub, _ = prepare_full_example_2()
You can pass both |Model| objects and names and, as a keyword
argument, the name of the newly created |Selection| object:
>>> test = pub.selections.complete.copy('test')
>>> from hydpy import prepare_model
>>> hland_v1 = prepare_model('hland_v1')
>>> test.search_modeltypes(hland_v1)
Selection("modeltypes",
nodes=(),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"land_lahn_3"))
>>> test.search_modeltypes(
... hland_v1, 'hstream_v1', 'lland_v1', name='MODELTYPES')
Selection("MODELTYPES",
nodes=(),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"land_lahn_3", "stream_dill_lahn_2",
"stream_lahn_1_lahn_2", "stream_lahn_2_lahn_3"))
Wrong model specifications result in errors like the following:
>>> test.search_modeltypes('wrong')
Traceback (most recent call last):
...
ModuleNotFoundError: While trying to determine the elements of \
selection `test` handling the model defined by the argument(s) `wrong` \
of type(s) `str`, the following error occurred: \
No module named 'hydpy.models.wrong'
Method |Selection.select_modeltypes| restricts the current selection to
the one determined with the method the |Selection.search_modeltypes|:
>>> test.select_modeltypes(hland_v1)
Selection("test",
nodes=(),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"land_lahn_3"))
On the contrary, the method |Selection.deselect_upstream| restricts
the current selection to all devices not determined by method the
|Selection.search_upstream|:
>>> pub.selections.complete.deselect_modeltypes(hland_v1)
Selection("complete",
nodes=(),
elements=("stream_dill_lahn_2", "stream_lahn_1_lahn_2",
"stream_lahn_2_lahn_3"))
""" |
try:
typelist = []
for model in models:
if not isinstance(model, modeltools.Model):
model = importtools.prepare_model(model)
typelist.append(type(model))
typetuple = tuple(typelist)
selection = Selection(name)
for element in self.elements:
if isinstance(element.model, typetuple):
selection.elements += element
return selection
except BaseException:
values = objecttools.enumeration(models)
classes = objecttools.enumeration(
objecttools.classname(model) for model in models)
objecttools.augment_excmessage(
f'While trying to determine the elements of selection '
f'`{self.name}` handling the model defined by the '
f'argument(s) `{values}` of type(s) `{classes}`') |
<SYSTEM_TASK:>
Return a new selection containing all nodes of the current
<END_TASK>
<USER_TASK:>
Description:
def search_nodenames(self, *substrings: str, name: str = 'nodenames') -> \
'Selection':
"""Return a new selection containing all nodes of the current
selection with a name containing at least one of the given substrings.
>>> from hydpy.core.examples import prepare_full_example_2
>>> hp, pub, _ = prepare_full_example_2()
Pass the (sub)strings as positional arguments and, optionally, the
name of the newly created |Selection| object as a keyword argument:
>>> test = pub.selections.complete.copy('test')
>>> from hydpy import prepare_model
>>> test.search_nodenames('dill', 'lahn_1')
Selection("nodenames",
nodes=("dill", "lahn_1"),
elements=())
Wrong string specifications result in errors like the following:
>>> test.search_nodenames(['dill', 'lahn_1'])
Traceback (most recent call last):
...
TypeError: While trying to determine the nodes of selection \
`test` with names containing at least one of the given substrings \
`['dill', 'lahn_1']`, the following error occurred: 'in <string>' \
requires string as left operand, not list
Method |Selection.select_nodenames| restricts the current selection
to the one determined with the the method |Selection.search_nodenames|:
>>> test.select_nodenames('dill', 'lahn_1')
Selection("test",
nodes=("dill", "lahn_1"),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"land_lahn_3", "stream_dill_lahn_2",
"stream_lahn_1_lahn_2", "stream_lahn_2_lahn_3"))
On the contrary, the method |Selection.deselect_nodenames| restricts
the current selection to all devices not determined by the method
|Selection.search_nodenames|:
>>> pub.selections.complete.deselect_nodenames('dill', 'lahn_1')
Selection("complete",
nodes=("lahn_2", "lahn_3"),
elements=("land_dill", "land_lahn_1", "land_lahn_2",
"land_lahn_3", "stream_dill_lahn_2",
"stream_lahn_1_lahn_2", "stream_lahn_2_lahn_3"))
""" |
try:
selection = Selection(name)
for node in self.nodes:
for substring in substrings:
if substring in node.name:
selection.nodes += node
break
return selection
except BaseException:
values = objecttools.enumeration(substrings)
objecttools.augment_excmessage(
f'While trying to determine the nodes of selection '
f'`{self.name}` with names containing at least one '
f'of the given substrings `{values}`') |
<SYSTEM_TASK:>
Return a new selection containing all elements of the current
<END_TASK>
<USER_TASK:>
Description:
def search_elementnames(self, *substrings: str,
name: str = 'elementnames') -> 'Selection':
"""Return a new selection containing all elements of the current
selection with a name containing at least one of the given substrings.
>>> from hydpy.core.examples import prepare_full_example_2
>>> hp, pub, _ = prepare_full_example_2()
Pass the (sub)strings as positional arguments and, optionally, the
name of the newly created |Selection| object as a keyword argument:
>>> test = pub.selections.complete.copy('test')
>>> from hydpy import prepare_model
>>> test.search_elementnames('dill', 'lahn_1')
Selection("elementnames",
nodes=(),
elements=("land_dill", "land_lahn_1", "stream_dill_lahn_2",
"stream_lahn_1_lahn_2"))
Wrong string specifications result in errors like the following:
>>> test.search_elementnames(['dill', 'lahn_1'])
Traceback (most recent call last):
...
TypeError: While trying to determine the elements of selection \
`test` with names containing at least one of the given substrings \
`['dill', 'lahn_1']`, the following error occurred: 'in <string>' \
requires string as left operand, not list
Method |Selection.select_elementnames| restricts the current selection
to the one determined with the method |Selection.search_elementnames|:
>>> test.select_elementnames('dill', 'lahn_1')
Selection("test",
nodes=("dill", "lahn_1", "lahn_2", "lahn_3"),
elements=("land_dill", "land_lahn_1", "stream_dill_lahn_2",
"stream_lahn_1_lahn_2"))
On the contrary, the method |Selection.deselect_elementnames|
restricts the current selection to all devices not determined
by the method |Selection.search_elementnames|:
>>> pub.selections.complete.deselect_elementnames('dill', 'lahn_1')
Selection("complete",
nodes=("dill", "lahn_1", "lahn_2", "lahn_3"),
elements=("land_lahn_2", "land_lahn_3",
"stream_lahn_2_lahn_3"))
""" |
try:
selection = Selection(name)
for element in self.elements:
for substring in substrings:
if substring in element.name:
selection.elements += element
break
return selection
except BaseException:
values = objecttools.enumeration(substrings)
objecttools.augment_excmessage(
f'While trying to determine the elements of selection '
f'`{self.name}` with names containing at least one '
f'of the given substrings `{values}`') |
<SYSTEM_TASK:>
Return a new |Selection| object with the given name and copies
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Description:
def copy(self, name: str) -> 'Selection':
"""Return a new |Selection| object with the given name and copies
of the handles |Nodes| and |Elements| objects based on method
|Devices.copy|.""" |
return type(self)(name, copy.copy(self.nodes), copy.copy(self.elements)) |
<SYSTEM_TASK:>
Save the selection as a network file.
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Description:
def save_networkfile(self, filepath: Union[str, None] = None,
write_nodes: bool = True) -> None:
"""Save the selection as a network file.
>>> from hydpy.core.examples import prepare_full_example_2
>>> _, pub, TestIO = prepare_full_example_2()
In most cases, one should conveniently write network files via method
|NetworkManager.save_files| of class |NetworkManager|. However,
using the method |Selection.save_networkfile| allows for additional
configuration via the arguments `filepath` and `write_nodes`:
>>> with TestIO():
... pub.selections.headwaters.save_networkfile()
... with open('headwaters.py') as networkfile:
... print(networkfile.read())
# -*- coding: utf-8 -*-
<BLANKLINE>
from hydpy import Node, Element
<BLANKLINE>
<BLANKLINE>
Node("dill", variable="Q",
keywords="gauge")
<BLANKLINE>
Node("lahn_1", variable="Q",
keywords="gauge")
<BLANKLINE>
<BLANKLINE>
Element("land_dill",
outlets="dill",
keywords="catchment")
<BLANKLINE>
Element("land_lahn_1",
outlets="lahn_1",
keywords="catchment")
<BLANKLINE>
>>> with TestIO():
... pub.selections.headwaters.save_networkfile('test.py', False)
... with open('test.py') as networkfile:
... print(networkfile.read())
# -*- coding: utf-8 -*-
<BLANKLINE>
from hydpy import Node, Element
<BLANKLINE>
<BLANKLINE>
Element("land_dill",
outlets="dill",
keywords="catchment")
<BLANKLINE>
Element("land_lahn_1",
outlets="lahn_1",
keywords="catchment")
<BLANKLINE>
""" |
if filepath is None:
filepath = self.name + '.py'
with open(filepath, 'w', encoding="utf-8") as file_:
file_.write('# -*- coding: utf-8 -*-\n')
file_.write('\nfrom hydpy import Node, Element\n\n')
if write_nodes:
for node in self.nodes:
file_.write('\n' + repr(node) + '\n')
file_.write('\n')
for element in self.elements:
file_.write('\n' + repr(element) + '\n') |
<SYSTEM_TASK:>
Calculate the input discharge portions of the different response
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Description:
def calc_qpin_v1(self):
"""Calculate the input discharge portions of the different response
functions.
Required derived parameters:
|Nmb|
|MaxQ|
|DiffQ|
Required flux sequence:
|QIn|
Calculated flux sequences:
|QPIn|
Examples:
Initialize an arma model with three different response functions:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb = 3
>>> derived.maxq.shape = 3
>>> derived.diffq.shape = 2
>>> fluxes.qpin.shape = 3
Define the maximum discharge value of the respective response
functions and their successive differences:
>>> derived.maxq(0.0, 2.0, 6.0)
>>> derived.diffq(2., 4.)
The first six examples are performed for inflow values ranging from
0 to 12 m³/s:
>>> from hydpy import UnitTest
>>> test = UnitTest(
... model, model.calc_qpin_v1,
... last_example=6,
... parseqs=(fluxes.qin, fluxes.qpin))
>>> test.nexts.qin = 0., 1., 2., 4., 6., 12.
>>> test()
| ex. | qin | qpin |
-------------------------------
| 1 | 0.0 | 0.0 0.0 0.0 |
| 2 | 1.0 | 1.0 0.0 0.0 |
| 3 | 2.0 | 2.0 0.0 0.0 |
| 4 | 4.0 | 2.0 2.0 0.0 |
| 5 | 6.0 | 2.0 4.0 0.0 |
| 6 | 12.0 | 2.0 4.0 6.0 |
The following two additional examples are just supposed to
demonstrate method |calc_qpin_v1| also functions properly if
there is only one response function, wherefore total discharge
does not need to be divided:
>>> derived.nmb = 1
>>> derived.maxq.shape = 1
>>> derived.diffq.shape = 0
>>> fluxes.qpin.shape = 1
>>> derived.maxq(0.)
>>> test = UnitTest(
... model, model.calc_qpin_v1,
... first_example=7, last_example=8,
... parseqs=(fluxes.qin,
... fluxes.qpin))
>>> test.nexts.qin = 0., 12.
>>> test()
| ex. | qin | qpin |
---------------------
| 7 | 0.0 | 0.0 |
| 8 | 12.0 | 12.0 |
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
for idx in range(der.nmb-1):
if flu.qin < der.maxq[idx]:
flu.qpin[idx] = 0.
elif flu.qin < der.maxq[idx+1]:
flu.qpin[idx] = flu.qin-der.maxq[idx]
else:
flu.qpin[idx] = der.diffq[idx]
flu.qpin[der.nmb-1] = max(flu.qin-der.maxq[der.nmb-1], 0.) |
<SYSTEM_TASK:>
Refresh the input log sequence for the different MA processes.
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Description:
def calc_login_v1(self):
"""Refresh the input log sequence for the different MA processes.
Required derived parameters:
|Nmb|
|MA_Order|
Required flux sequence:
|QPIn|
Updated log sequence:
|LogIn|
Example:
Assume there are three response functions, involving one, two and
three MA coefficients respectively:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(3)
>>> derived.ma_order.shape = 3
>>> derived.ma_order = 1, 2, 3
>>> fluxes.qpin.shape = 3
>>> logs.login.shape = (3, 3)
The "memory values" of the different MA processes are defined as
follows (one row for each process):
>>> logs.login = ((1.0, nan, nan),
... (2.0, 3.0, nan),
... (4.0, 5.0, 6.0))
These are the new inflow discharge portions to be included into
the memories of the different processes:
>>> fluxes.qpin = 7.0, 8.0, 9.0
Through applying method |calc_login_v1| all values already
existing are shifted to the right ("into the past"). Values,
which are no longer required due to the limited order or the
different MA processes, are discarded. The new values are
inserted in the first column:
>>> model.calc_login_v1()
>>> logs.login
login([[7.0, nan, nan],
[8.0, 2.0, nan],
[9.0, 4.0, 5.0]])
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
log = self.sequences.logs.fastaccess
for idx in range(der.nmb):
for jdx in range(der.ma_order[idx]-2, -1, -1):
log.login[idx, jdx+1] = log.login[idx, jdx]
for idx in range(der.nmb):
log.login[idx, 0] = flu.qpin[idx] |
<SYSTEM_TASK:>
Calculate the discharge responses of the different MA processes.
<END_TASK>
<USER_TASK:>
Description:
def calc_qma_v1(self):
"""Calculate the discharge responses of the different MA processes.
Required derived parameters:
|Nmb|
|MA_Order|
|MA_Coefs|
Required log sequence:
|LogIn|
Calculated flux sequence:
|QMA|
Examples:
Assume there are three response functions, involving one, two and
three MA coefficients respectively:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(3)
>>> derived.ma_order.shape = 3
>>> derived.ma_order = 1, 2, 3
>>> derived.ma_coefs.shape = (3, 3)
>>> logs.login.shape = (3, 3)
>>> fluxes.qma.shape = 3
The coefficients of the different MA processes are stored in
separate rows of the 2-dimensional parameter `ma_coefs`:
>>> derived.ma_coefs = ((1.0, nan, nan),
... (0.8, 0.2, nan),
... (0.5, 0.3, 0.2))
The "memory values" of the different MA processes are defined as
follows (one row for each process). The current values are stored
in first column, the values of the last time step in the second
column, and so on:
>>> logs.login = ((1.0, nan, nan),
... (2.0, 3.0, nan),
... (4.0, 5.0, 6.0))
Applying method |calc_qma_v1| is equivalent to calculating the
inner product of the different rows of both matrices:
>>> model.calc_qma_v1()
>>> fluxes.qma
qma(1.0, 2.2, 4.7)
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
log = self.sequences.logs.fastaccess
for idx in range(der.nmb):
flu.qma[idx] = 0.
for jdx in range(der.ma_order[idx]):
flu.qma[idx] += der.ma_coefs[idx, jdx] * log.login[idx, jdx] |
<SYSTEM_TASK:>
Calculate the discharge responses of the different AR processes.
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<USER_TASK:>
Description:
def calc_qar_v1(self):
"""Calculate the discharge responses of the different AR processes.
Required derived parameters:
|Nmb|
|AR_Order|
|AR_Coefs|
Required log sequence:
|LogOut|
Calculated flux sequence:
|QAR|
Examples:
Assume there are four response functions, involving zero, one, two,
and three AR coefficients respectively:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(4)
>>> derived.ar_order.shape = 4
>>> derived.ar_order = 0, 1, 2, 3
>>> derived.ar_coefs.shape = (4, 3)
>>> logs.logout.shape = (4, 3)
>>> fluxes.qar.shape = 4
The coefficients of the different AR processes are stored in
separate rows of the 2-dimensional parameter `ma_coefs`.
Note the special case of the first AR process of zero order
(first row), which involves no autoregressive memory at all:
>>> derived.ar_coefs = ((nan, nan, nan),
... (1.0, nan, nan),
... (0.8, 0.2, nan),
... (0.5, 0.3, 0.2))
The "memory values" of the different AR processes are defined as
follows (one row for each process). The values of the last time
step are stored in first column, the values of the last time step
in the second column, and so on:
>>> logs.logout = ((nan, nan, nan),
... (1.0, nan, nan),
... (2.0, 3.0, nan),
... (4.0, 5.0, 6.0))
Applying method |calc_qar_v1| is equivalent to calculating the
inner product of the different rows of both matrices:
>>> model.calc_qar_v1()
>>> fluxes.qar
qar(0.0, 1.0, 2.2, 4.7)
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
log = self.sequences.logs.fastaccess
for idx in range(der.nmb):
flu.qar[idx] = 0.
for jdx in range(der.ar_order[idx]):
flu.qar[idx] += der.ar_coefs[idx, jdx] * log.logout[idx, jdx] |
<SYSTEM_TASK:>
Calculate the ARMA results for the different response functions.
<END_TASK>
<USER_TASK:>
Description:
def calc_qpout_v1(self):
"""Calculate the ARMA results for the different response functions.
Required derived parameter:
|Nmb|
Required flux sequences:
|QMA|
|QAR|
Calculated flux sequence:
|QPOut|
Examples:
Initialize an arma model with three different response functions:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(3)
>>> fluxes.qma.shape = 3
>>> fluxes.qar.shape = 3
>>> fluxes.qpout.shape = 3
Define the output values of the MA and of the AR processes
associated with the three response functions and apply
method |calc_qpout_v1|:
>>> fluxes.qar = 4.0, 5.0, 6.0
>>> fluxes.qma = 1.0, 2.0, 3.0
>>> model.calc_qpout_v1()
>>> fluxes.qpout
qpout(5.0, 7.0, 9.0)
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
for idx in range(der.nmb):
flu.qpout[idx] = flu.qma[idx]+flu.qar[idx] |
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Refresh the log sequence for the different AR processes.
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Description:
def calc_logout_v1(self):
"""Refresh the log sequence for the different AR processes.
Required derived parameters:
|Nmb|
|AR_Order|
Required flux sequence:
|QPOut|
Updated log sequence:
|LogOut|
Example:
Assume there are four response functions, involving zero, one, two
and three AR coefficients respectively:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(4)
>>> derived.ar_order.shape = 4
>>> derived.ar_order = 0, 1, 2, 3
>>> fluxes.qpout.shape = 4
>>> logs.logout.shape = (4, 3)
The "memory values" of the different AR processes are defined as
follows (one row for each process). Note the special case of the
first AR process of zero order (first row), which is why there are
no autoregressive memory values required:
>>> logs.logout = ((nan, nan, nan),
... (0.0, nan, nan),
... (1.0, 2.0, nan),
... (3.0, 4.0, 5.0))
These are the new outflow discharge portions to be included into
the memories of the different processes:
>>> fluxes.qpout = 6.0, 7.0, 8.0, 9.0
Through applying method |calc_logout_v1| all values already
existing are shifted to the right ("into the past"). Values, which
are no longer required due to the limited order or the different
AR processes, are discarded. The new values are inserted in the
first column:
>>> model.calc_logout_v1()
>>> logs.logout
logout([[nan, nan, nan],
[7.0, nan, nan],
[8.0, 1.0, nan],
[9.0, 3.0, 4.0]])
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
log = self.sequences.logs.fastaccess
for idx in range(der.nmb):
for jdx in range(der.ar_order[idx]-2, -1, -1):
log.logout[idx, jdx+1] = log.logout[idx, jdx]
for idx in range(der.nmb):
if der.ar_order[idx] > 0:
log.logout[idx, 0] = flu.qpout[idx] |
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Sum up the results of the different response functions.
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Description:
def calc_qout_v1(self):
"""Sum up the results of the different response functions.
Required derived parameter:
|Nmb|
Required flux sequences:
|QPOut|
Calculated flux sequence:
|QOut|
Examples:
Initialize an arma model with three different response functions:
>>> from hydpy.models.arma import *
>>> parameterstep()
>>> derived.nmb(3)
>>> fluxes.qpout.shape = 3
Define the output values of the three response functions and
apply method |calc_qout_v1|:
>>> fluxes.qpout = 1.0, 2.0, 3.0
>>> model.calc_qout_v1()
>>> fluxes.qout
qout(6.0)
""" |
der = self.parameters.derived.fastaccess
flu = self.sequences.fluxes.fastaccess
flu.qout = 0.
for idx in range(der.nmb):
flu.qout += flu.qpout[idx] |
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Determine the number of branches
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Description:
def update(self):
"""Determine the number of branches""" |
con = self.subpars.pars.control
self(con.ypoints.shape[0]) |
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Update value based on the actual |calc_qg_v1| method.
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Description:
def update(self):
"""Update value based on the actual |calc_qg_v1| method.
Required derived parameter:
|H|
Note that the value of parameter |lstream_derived.QM| is directly
related to the value of parameter |HM| and indirectly related to
all parameters values relevant for method |calc_qg_v1|. Hence the
complete paramter (and sequence) requirements might differ for
various application models.
For examples, see the documentation on method ToDo.
""" |
mod = self.subpars.pars.model
con = mod.parameters.control
flu = mod.sequences.fluxes
flu.h = con.hm
mod.calc_qg()
self(flu.qg) |
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Determines in how many segments the whole reach needs to be
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Description:
def update(self):
"""Determines in how many segments the whole reach needs to be
divided to approximate the desired lag time via integer rounding.
Adjusts the shape of sequence |QJoints| additionally.
Required control parameters:
|Lag|
Calculated derived parameters:
|NmbSegments|
Prepared state sequence:
|QJoints|
Examples:
Define a lag time of 1.4 days and a simulation step size of 12
hours:
>>> from hydpy.models.hstream import *
>>> parameterstep('1d')
>>> simulationstep('12h')
>>> lag(1.4)
Then the actual lag value for the simulation step size is 2.8
>>> lag
lag(1.4)
>>> lag.value
2.8
Through rounding the number of segments is determined:
>>> derived.nmbsegments.update()
>>> derived.nmbsegments
nmbsegments(3)
The number of joints is always the number of segments plus one:
>>> states.qjoints.shape
(4,)
""" |
pars = self.subpars.pars
self(int(round(pars.control.lag)))
pars.model.sequences.states.qjoints.shape = self+1 |
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View the supplied data in an interactive, graphical table widget.
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Description:
def view(data, enc=None, start_pos=None, delimiter=None, hdr_rows=None,
idx_cols=None, sheet_index=0, transpose=False, wait=None,
recycle=None, detach=None, metavar=None, title=None):
"""View the supplied data in an interactive, graphical table widget.
data: When a valid path or IO object, read it as a tabular text file. When
a valid URI, a Blaze object is constructed and visualized. Any other
supported datatype is visualized directly and incrementally *without
copying*.
enc: File encoding (such as "utf-8", normally autodetected).
delimiter: Text file delimiter (normally autodetected).
hdr_rows: For files or lists of lists, specify the number of header rows.
For files only, a default of one header line is assumed.
idx_cols: For files or lists of lists, specify the number of index columns.
By default, no index is assumed.
sheet_index: For multi-table files (such as xls[x]), specify the sheet
index to read, starting from 0. Defaults to the first.
start_pos: A tuple of the form (y, x) specifying the initial cursor
position. Negative offsets count from the end of the dataset.
transpose: Transpose the resulting view.
metavar: name of the variable being shown for display purposes (inferred
automatically when possible).
title: title of the data window.
wait: Wait for the user to close the view before returning. By default, try
to match the behavior of ``matplotlib.is_interactive()``. If
matplotlib is not loaded, wait only if ``detach`` is also False. The
default value can also be set through ``gtabview.WAIT``.
recycle: Recycle the previous window instead of creating a new one. The
default is True, and can also be set through ``gtabview.RECYCLE``.
detach: Create a fully detached GUI thread for interactive use (note: this
is *not* necessary if matplotlib is loaded). The default is False,
and can also be set through ``gtabview.DETACH``.
""" |
global WAIT, RECYCLE, DETACH, VIEW
model = read_model(data, enc=enc, delimiter=delimiter, hdr_rows=hdr_rows,
idx_cols=idx_cols, sheet_index=sheet_index,
transpose=transpose)
if model is None:
warnings.warn("cannot visualize the supplied data type: {}".format(type(data)),
category=RuntimeWarning)
return None
# setup defaults
if wait is None: wait = WAIT
if recycle is None: recycle = RECYCLE
if detach is None: detach = DETACH
if wait is None:
if 'matplotlib' not in sys.modules:
wait = not bool(detach)
else:
import matplotlib.pyplot as plt
wait = not plt.isinteractive()
# try to fetch the variable name in the upper stack
if metavar is None:
if isinstance(data, basestring):
metavar = data
else:
metavar = _varname_in_stack(data, 1)
# create a view controller
if VIEW is None:
if not detach:
VIEW = ViewController()
else:
VIEW = DetachedViewController()
VIEW.setDaemon(True)
VIEW.start()
if VIEW.is_detached():
atexit.register(VIEW.exit)
else:
VIEW = None
return None
# actually show the data
view_kwargs = {'hdr_rows': hdr_rows, 'idx_cols': idx_cols,
'start_pos': start_pos, 'metavar': metavar, 'title': title}
VIEW.view(model, view_kwargs, wait=wait, recycle=recycle)
return VIEW |
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Get and clear the current |Node| and |Element| registries.
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Description:
def gather_registries() -> Tuple[Dict, Mapping, Mapping]:
"""Get and clear the current |Node| and |Element| registries.
Function |gather_registries| is thought to be used by class |Tester| only.
""" |
id2devices = copy.copy(_id2devices)
registry = copy.copy(_registry)
selection = copy.copy(_selection)
dict_ = globals()
dict_['_id2devices'] = {}
dict_['_registry'] = {Node: {}, Element: {}}
dict_['_selection'] = {Node: {}, Element: {}}
return id2devices, registry, selection |
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Reset the current |Node| and |Element| registries.
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Description:
def reset_registries(dicts: Tuple[Dict, Mapping, Mapping]):
"""Reset the current |Node| and |Element| registries.
Function |reset_registries| is thought to be used by class |Tester| only.
""" |
dict_ = globals()
dict_['_id2devices'] = dicts[0]
dict_['_registry'] = dicts[1]
dict_['_selection'] = dicts[2] |
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Return a list of all keywords starting with the given string.
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Description:
def startswith(self, name: str) -> List[str]:
"""Return a list of all keywords starting with the given string.
>>> from hydpy.core.devicetools import Keywords
>>> keywords = Keywords('first_keyword', 'second_keyword',
... 'keyword_3', 'keyword_4',
... 'keyboard')
>>> keywords.startswith('keyword')
['keyword_3', 'keyword_4']
""" |
return sorted(keyword for keyword in self if keyword.startswith(name)) |
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Return a list of all keywords ending with the given string.
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Description:
def endswith(self, name: str) -> List[str]:
"""Return a list of all keywords ending with the given string.
>>> from hydpy.core.devicetools import Keywords
>>> keywords = Keywords('first_keyword', 'second_keyword',
... 'keyword_3', 'keyword_4',
... 'keyboard')
>>> keywords.endswith('keyword')
['first_keyword', 'second_keyword']
""" |
return sorted(keyword for keyword in self if keyword.endswith(name)) |
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Return a list of all keywords containing the given string.
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Description:
def contains(self, name: str) -> List[str]:
"""Return a list of all keywords containing the given string.
>>> from hydpy.core.devicetools import Keywords
>>> keywords = Keywords('first_keyword', 'second_keyword',
... 'keyword_3', 'keyword_4',
... 'keyboard')
>>> keywords.contains('keyword')
['first_keyword', 'keyword_3', 'keyword_4', 'second_keyword']
""" |
return sorted(keyword for keyword in self if name in keyword) |
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