Genesis and maintenance of "Mediterranean hurricanes"

Cyclonic storms that closely resemble tropical cyclones in satellite images occasionally form over the Mediterranean Sea. Synoptic and mesoscale analyses of such storms show small, warm-core structure and surface winds sometimes exceeding 25ms<sup>-1</sup> over small areas. These analyse...

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Main Author: K. Emanuel
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/2/217/2005/adgeo-2-217-2005.pdf
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author K. Emanuel
author_facet K. Emanuel
author_sort K. Emanuel
collection DOAJ
description Cyclonic storms that closely resemble tropical cyclones in satellite images occasionally form over the Mediterranean Sea. Synoptic and mesoscale analyses of such storms show small, warm-core structure and surface winds sometimes exceeding 25ms<sup>-1</sup> over small areas. These analyses, together with numerical simulations, reveal that in their mature stages, such storms intensify and are maintained by a feedback between surface enthalpy fluxes and wind, and as such are isomorphic with tropical cyclones. In this paper, I demonstrate that a cold, upper low over the Mediterranean can produce strong cyclogenesis in an axisymmetric model, thereby showing that baroclinic instability is not necessary during the mature stages of Mediterranean hurricanes.
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spelling doaj.art-69c5ee7a4a6f4b4ab3d52705677d1ddc2022-12-22T01:18:52ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592005-01-012217220Genesis and maintenance of &quot;Mediterranean hurricanes&quot;K. EmanuelCyclonic storms that closely resemble tropical cyclones in satellite images occasionally form over the Mediterranean Sea. Synoptic and mesoscale analyses of such storms show small, warm-core structure and surface winds sometimes exceeding 25ms<sup>-1</sup> over small areas. These analyses, together with numerical simulations, reveal that in their mature stages, such storms intensify and are maintained by a feedback between surface enthalpy fluxes and wind, and as such are isomorphic with tropical cyclones. In this paper, I demonstrate that a cold, upper low over the Mediterranean can produce strong cyclogenesis in an axisymmetric model, thereby showing that baroclinic instability is not necessary during the mature stages of Mediterranean hurricanes.http://www.adv-geosci.net/2/217/2005/adgeo-2-217-2005.pdf
spellingShingle K. Emanuel
Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
Advances in Geosciences
title Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
title_full Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
title_fullStr Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
title_full_unstemmed Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
title_short Genesis and maintenance of &quot;Mediterranean hurricanes&quot;
title_sort genesis and maintenance of quot mediterranean hurricanes quot
url http://www.adv-geosci.net/2/217/2005/adgeo-2-217-2005.pdf
work_keys_str_mv AT kemanuel genesisandmaintenanceofquotmediterraneanhurricanesquot