Boundary-layer friction in midlatitude cyclones

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Boundary-layer friction in midlatitude cyclones

Results from an idealized three-dimensional baroclinic life-cycle model are interpreted in a potential vorticity (PV) framework to identify the physical mechanisms by which frictional processes acting in the atmospheric boundary layer modify and reduce the baroclinic development of a midlatitude storm. Considering a life cycle where the only non-conservative process acting is boundary-layer fri...

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ژورنال

عنوان ژورنال: Quarterly Journal of the Royal Meteorological Society

سال: 2006

ISSN: 0035-9009,1477-870X

DOI: 10.1256/qj.04.145