A note on boundary-layer friction in baroclinic cyclones

Details A note on boundary-layer friction in baroclinic cyclones A note on boundary-layer friction in baroclinic cyclones

2008-01-30

arxiv.org/abs/0801.4648v1

Quarterly Journal of the Royal Meteorological Society, 133, 2137-2141 (2007)

Physics

Atmospheric and Oceanic Physics

5 pages, 3 figures

Scientific paper

10.1002/qj.179

The interaction between extratropical cyclones and the underlying boundary layer has been a topic of recent discussion in papers by Adamson et. al. (2006) and Beare (2007). Their results emphasise different mechanisms through which the boundary layer dynamics may modify the growth of a baroclinic cyclone. By using different sea-surface temperature distributions and comparing the low-level winds, the differences are exposed and both of the proposed mechanisms appear to be acting within a single simulation.

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