A note on boundary layer friction in baroclinic cyclonesBoutle, I. A., Beare, R. J., Belcher, S. E. and Plant, R. S. ORCID: https://orcid.org/0000-0001-8808-0022 (2007) A note on boundary layer friction in baroclinic cyclones. Quarterly Journal of the Royal Meteorological Society, 133. pp. 2137-2141. ISSN 1477-870X Full text not archived in this repository. It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing. To link to this item DOI: 10.1002/qj.179 Abstract/SummaryThe 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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