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Fig2.1.3.1-1: ENS grid points over part of southern England.  Within each box all locations are considered to have the same values as forecast at the central grid point.  The fluxes of heat, moisture and momentum at the grid point are calculated using the proportion of land (where the HTESSEL is used) and sea (shallow coastal sub-grid scale waters where FLake is used).  Where the land fraction is <50% NEMO is used to provide oceanic fluxes unless the lake dataset specifically highlights the location as a lake (e.g. the Great Lakes) when FLake is used.

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