hydromt_wflow.WflowModel.setup_cold_states#
- WflowModel.setup_cold_states(timestamp: str = None) None [source]#
Prepare cold states for Wflow.
To be run last as this requires some soil parameters or constant_pars to be computed already.
To be run after setup_lakes, setup_reservoirs and setup_glaciers to also create cold states for them if they are present in the basin.
This function is mainly useful in case the wflow model is read into Delft-FEWS.
Adds model layers:
soil_saturated_depth: saturated store [mm]
snow_leq_depth: snow storage [mm]
soil_temp: top soil temperature [°C]
soil_unsaturated_depth: amount of water in the unsaturated store, per layer [mm]
snow_water_depth: liquid water content in the snow pack [mm]
vegetation_water_depth: canopy storage [mm]
river_instantaneous_q: river discharge [m3/s]
river_instantaneous_h: river water level [m]
subsurface_q: subsurface flow [m3/d]
land_instantaneous_h: land water level [m]
land_instantaneous_q or land_instantaneous_qx**+ **land_instantaneous_qy: overland flow for kinwave [m3/s] or overland flow in x/y directions for local-inertial [m3/s]
If lakes, also adds:
lake_instantaneous_water_level: lake water level [m]
If reservoirs, also adds:
reservoir_instantaneous_volume: reservoir volume [m3]
If glaciers, also adds:
glacier_leq_depth: water within the glacier [mm]
If paddy, also adds:
demand_paddy_h: water on the paddy fields [mm]
- Parameters:
timestamp (str, optional) – Timestamp of the cold states. By default uses the (starttime - timestepsecs) from the config.