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Variable Infiltration Capacity (VIC) model

The benefits

In short
  • Solves equations
  • Vegetation and elevation variability
  • Evapotranspiration modeling
  • Runoff routing
  • Flexible configuration

VIC is a grid-based macro-scale hydrological model that solves both the surface energy and the water balance, representing sub-grid variability in vegetation and elevation for large-scale hydrological studies

The Variable Infiltration Capacity (VIC) model (Liang et al., 1994) is a grid-based macro-scale hydrological model that solves both the surface energy balance and water balance equations. Each grid cell is partitioned into multiple land cover and elevation classes, with the soil column commonly divided into three soil layers. Evapotranspiration is calculated based on the Penman-Monteith equation (Monteith, 1965; Penman, 1948). Surface runoff in the upper soil layer is based on the variable infiltration curve (Zhao et al., 1980), and baseflow release from the lowest soil layer follows the non-linear Arno recession curve (Todini, 1996). Runoff and baseflow are routed along stream networks with an offline routing model using the unit hydrograph principle and linearized St. Venant’s equations (Lohmann et al., 1998). Within the Water Systems and Global Change group, VIC has been applied in global (Haddeland et al., 2014; van Vliet et al., 2013, 2016), European (Greuell et al., 2015), and seasonal forecasting studies (Greuell et al., 2016).

Figure: Concept of VIC macro-scale hydrological model (source: VIC-website University of Washington)

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Selection of main publications