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Hamish A. Ramsay, Lance M. Leslie, and Jeffrey D. Kepert

model includes a choice of parameterizations for the surface layer and turbulent closure. For these calculations, the surface layer parameterization used Monin–Obukhov similarity theory with the momentum roughness given by a Charnock (1955) relation and the heat and moisture roughness lengths after Liu et al. (1979) , with a Mellor–Yamada level-2.25 closure ( Galperin et al. 1988 ) for levels above that. These parameterizations are similar to those used for the MM5 runs, and it is not expected

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