RechargeModel#
- class RechargeModel(prec, evap, rfunc=None, name='recharge', recharge=None, temp=None, settings=('prec', 'evap', 'evap'), metadata=(None, None, None))[source]#
Stressmodel simulating the effect of groundwater recharge on the head.
- Parameters
prec (pandas.Series) – pandas.Series with pandas.DatetimeIndex containing the precipitation series. The precipitation series should be provided in mm/day when a nonlinear model is used.
evap (pandas.Series) – pandas.Series with pandas.DatetimeIndex containing the potential evaporation series. The evaporation series should be provided in mm/day when a nonlinear model is used.
rfunc (pastas.rfunc instance, optional) – Instance of the response function used in the convolution with the stress. Default is ps.Exponential().
name (str, optional) – Name of the stress. Default is “recharge”.
recharge (pastas.recharge instance, optional) – Instance of a recharge model. Options are: Linear, FlexModel and Berendrecht. These can be accessed through ps.rch. Default is ps.rch.Linear().
temp (pandas.Series, optional) – pandas.Series with pandas.DatetimeIndex containing the temperature series. It depends on the recharge model if this argument is required or not. The temperature series should be provided in degrees Celsius.
settings (list of dicts or str, optional) – The settings of the precipitation, evaporation and optionally temperature time series, in this order. By default (“prec”, “evap”, “evap”). This can be a string referring to a predefined settings dict (defined in ps.rcParams[“timeseries”]), or a dict with the settings to apply. For more information refer to Time Series Settings section below for more information.
metadata (tuple of dicts or list of dicts, optional) – dictionary containing metadata about the stress. This is passed onto the TimeSeries object.
Examples
>>> sm = ps.RechargeModel(rain, evap, rfunc=ps.Exponential(), >>> recharge=ps.rch.FlexModel(), name="rch") >>> ml.add_stressmodel(sm)
- Time series settings
fill_nan ({“drop”, “mean”, “interpolate”} or float) –
- Method for filling NaNs.
drop: drop NaNs from time series
mean: fill NaNs with mean value of time series
interpolate: fill NaNs by interpolating between finite values
float: fill NaN with provided value, e.g. 0.0
fill_before ({“mean”, “bfill”} or float) –
- Method for extending time series into past.
mean: extend time series into past with mean value of time series
bfill: extend time series into past by back-filling first value
float: extend time series into past with provided value, e.g. 0.0
fill_after ({“mean”, “ffill”} or float) –
- Method for extending time series into future.
mean: extend time series into future with mean value of time series
ffill: extend time series into future by forward-filling last value
float: extend time series into future with provided value, e.g. 0.0
sample_up ({“mean”, “interpolate”, “divide”} or float) – Method for up-sampling time series (increasing frequency, e.g. going from weekly to daily values).
bfill or backfill: fill up-sampled time steps by back-filling current values
ffill or pad: fill up-sampled time steps by forward-filling current values
mean: fill up-sampled time steps with mean of timeseries
interpolate: fill up-sampled time steps by interpolating between current values
divide: fill up-sampled steps with current value divided by length of current time steps (i.e. spread value over new time steps).
sample_down ({“mean”, “drop”, “sum”, “min”, “max”}) – Method for down-sampling time series (decreasing frequency, e.g. going from daily to weekly values).
mean: resample time series by taking the mean
drop: resample the time series by taking the mean, dropping any NaN-values
sum: resample time series by summing values
max: resample time series with maximum value
min: resample time series with minimum value
- Parameters
Notes
This stress model computes the contribution of precipitation and potential evaporation in two steps. In the first step a recharge flux is computed by a model determined by the input argument recharge. In the second step this recharge flux is convolved with a response function to obtain the contribution of recharge to the groundwater levels. If a nonlinear recharge model is used, the precipitation should be in mm/d.
Warning
We recommend not to store a RechargeModel is a variable named rm. This name is already reserved in IPython to remove files and will cause problems later.
- Raises
A warning if the the maximum annual precipitation is smaller than 12 and a –
nonlinear recharge model is applied. This is likely an indication that the units of –
the precipitation series are in m/d instead of mm/d. Please check the units of the –
precipitation series. –
- Parameters
Attributes#
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Methods#
Determine in how many time series the contribution can be split. |
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Get parameters and return as array. |
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Method to obtain the settings of the stresses. |
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Method to obtain the recharge stress calculated by the model. |
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Method to obtain the water balance components. |
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Internal method to set the initial parameters. |
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Method to simulate the contribution of recharge to the head. |
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Method to export the RechargeModel object. |
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Method to update the settings of the all stresses in the stress model. |