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Lin et al., 1983 [60] and Rutledge and Hobbs, 1984 [87].
t_{land}=dw_{land}(\frac{A_{r}}{10^{10}})^{0.25}
t_{ocean}=dw_{ocean}(\frac{A_{r}}{10^{10}})^{0.25}
where A_{r} is cell area. dw_{land}=0.20 and dw_{ocean}=0.10 are base value for sub-grid variability over land and ocean. The total horizontal sub-grid variability is:h_{var}=t_{land}\times fr_{land}+t_{ocean}\times (1-fr_{land})
h_{var}=min[0.2,max(0.01,h_{var})]
References cs_profile().
Referenced by terminal_fall(), and warm_rain().