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PaHM generates its fields such that the wind speeds outside the last closed isobar are set to zero while, the atmospheric pressure is set equal to some background pressure value. In coastal/regional and storm surge applications it is important to have a full forcing atmospheric field across the computational domain so "far-field" physical properties are accounted for.
It is therefore, a requirement that the voids in the PaHM generated wind fields to be filled with background wind data that could come from other external atmospheric databases (e.g., GFS, CFS, HWRF and others). The data should be blended with the PaHM generated fields to produce a unified wind field over the computational domain.
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