new_hydrobudget

Make a new HydroBudget object, by providing the calibration parameters for the
model computation.

HydroBudget is a spatially distributed
groundwater recharge model that computes a superficial water
budget on grid cells with outputs aggregated into monthly time steps.
It was developed as an accessible and computationally affordable model
to simulate groundwater recharge over large areas (thousands of km2,
regional-scale watersheds) and for long time periods (decades), in cold
and humid climates. Model algorithms are based on the research of
Dubois, E. et al. (2021a) <doi:10.5683/SP3/EUDV3H> and
Dubois, E. et al. (2021b) <doi:10.5194/hess-25-6567-2021>.

Yannick Marcon

rechaRge

HydroBudget – Groundwater Recharge Model

Emmanuel Dubois

new_hydrobudget function

<dl><dt>T_m</dt>
<dd>The melting temperature (°C)</dd>
<dt>C_m</dt>
<dd>The melting coefficient (mm/°C/d)</dd>
<dt>TT_F</dt>
<dd>The Threshold temperature for soil frost (°C)</dd>
<dt>F_T</dt>
<dd>The freezing time (d)</dd>
<dt>t_API</dt>
<dd>The antecedent precipitation index time (d)</dd>
<dt>f_runoff</dt>
<dd>The runoff factor (-)</dd>
<dt>sw_m</dt>
<dd>The maximum soil water content (mm)</dd>
<dt>f_inf</dt>
<dd>The infiltration factor (-)</dd></dl>

Arguments

HydroBudget object — new_hydrobudget

<dl>

<dt>T_m</dt>
<dd>The melting temperature (°C)</dd>


<dt>C_m</dt>
<dd>The melting coefficient (mm/°C/d)</dd>


<dt>TT_F</dt>
<dd>The Threshold temperature for soil frost (°C)</dd>


<dt>F_T</dt>
<dd>The freezing time (d)</dd>


<dt>t_API</dt>
<dd>The antecedent precipitation index time (d)</dd>


<dt>f_runoff</dt>
<dd>The runoff factor (-)</dd>


<dt>sw_m</dt>
<dd>The maximum soil water content (mm)</dd>


<dt>f_inf</dt>
<dd>The infiltration factor (-)</dd>

</dl>

new_hydrobudget: HydroBudget object

Description

Usage

Value

Arguments