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- W2010804722 abstract "Abstract A recently published slab model formulation of lake thermodynamics (Goyette et al., 2000), including an empirical factor to adjust the incoming heat flux so that the modelled lake surface temperature agrees with observed climatology, leads to a distinct lack of energy conservation. The empirical adjustment conceptually represents an exchange of heat between the mixed‐layer water (the slab that is explicitly simulated in the model) and deeper layers of water. It ensures a realistic temporal progression of temperature in the mixed layer, but the thermodynamic balance of the deeper water is not considered. When the deeper water is considered, it is found that the empirical adjustment accounts for the entire heat input to the deeper water, and on an annual mean basis, it is considerably unbalanced. This reveals a flaw in this model concept and, although not entirely invalidating the model, it needs to be included as a caveat in its use." @default.
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- W2010804722 date "2001-12-01" @default.
- W2010804722 modified "2023-09-25" @default.
- W2010804722 title "Comment on “application of the Canadian regional climate model to the Laurentian Great Lakes region: Implementation of a lake model”" @default.
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- W2010804722 doi "https://doi.org/10.1080/07055900.2001.9649691" @default.
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