Item talk:Q336684
From geokb
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SOILWAT2 is a process-based ecosystem water balance simulation model with a daily time step, multiple soil layers, snowpack dynamics, multiple vegetation types responsive to atmospheric CO2 concentrations, and hydraulic redistribution.
Inputs to SOILWAT2 include local meteorology (daily temperature and precipitation, mean monthly relative humidity, wind speed and cloud cover), vegetation (monthly total biomass, % live biomass, surface litter, belowground rooting profile) and soil texture (density, gravel, sand, silt, and clay) to simulate daily ecosystem water balance. SOILWAT2 simulates precipitation interception by vegetation and litter, evaporation of intercepted water, snowmelt, sublimation and wind redistribution of snow, surface ponding, moisture infiltration, saturated and unsaturated percolation and hydraulic redistribution for each soil layer, bare-soil evaporation, transpiration (CO2 sensitive), and deep drainage. Additionally, SOILWAT2 tracks daily changes in soil temperature in each layer of the soil profile. SOILWAT2 contains of six major modules: atmosphere, vegetation, precipitation, vertical soil water movement, evapotranspiration, and soil temperature.
Successful model applications cover global (e.g., Bradford et al., 2017; Schlaepfer et al., 2017; Tietjen et al., 2017) and North American dryland ecosystems (e.g., Bradford et al., 2020; Petrie et al., 2020) including dry grasslands (e.g., Bradford, Schlaepfer, Lauenroth, et al., 2014; Copeland et al., 2022; Lauenroth et al., 2014), dry forests (e.g., Bradford, Schlaepfer, & Lauenroth, 2014; Petrie et al., 2017), and shrublands (e.g., Palmquist et al., 2016a; Renne et al., 2019; Schlaepfer et al., 2012b, 2021) including simulations under climate change projections (e.g., Bradford et al., 2019, 2020; Palmquist et al., 2016b; Schlaepfer et al., 2012a, 2015, 2021).
SOILWAT2 is also used as the ecohydrological module for the individual-plant dynamics simulation model STEPWAT2 (e.g., Palmquist et al., 2018, 2021).
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