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VIC can use either the approximate soil temperature profile of [Liang et al. (1999)](../Documentation/References.md#primary-historical-reference) or a finite difference solution that takes soil ice content into account, vis a vis [Cherkauer and Lettenmaier (1999)](../Documentation/References.md#primary-historical-reference).
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These apply to the case QUICK_FLUX = FALSE and FROZEN_SOIL = TRUE, i.e. the formulation of [Cherkauer and Lettenmaier (1999)](../Documentation/References.md#primary-historical-reference).
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The lake/wetland model ([Bowling and Lettenmaier, 2010](../Documentation/References.md#primary-historical-reference)) handles the impoundment of surface water within a grid cell. Each grid cell is allowed to have a lake/wetland system contained within one of its landcover tiles. Here, a **_lake_** refers to any impounded surface water, including permanent lakes and seasonal flooding of vegetated land. The lake's area can vary with time as a function of storage and topography (bathymetry). In this context, **_wetland_** refers to the exposed portion of the landcover tile.
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#### Lake Model
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### Lake Model
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- Multi-layer lake model, based on the model of Hostetler and Bartlein (1990), Hostetler (1991), and Hostetler et al (2000)
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- Energy balance model
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####Wetland Model
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### Wetland Model
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- Lakes and wetlands exist in their own "tile" within the grid cell
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- Dynamic wetland area = tile area - dynamic lake area
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