Affiliation:
1. Departamento de Ciencias Ambientales Facultad de Ciencias Ambientales y Bioquímica Universidad de Castilla la Mancha Cuenca Spain
2. Agencia Estatal de Meteorología (AEMET) Department of Development and Applications Madrid Spain
3. Department of Earth and Geoenvironmental Sciences University of Bari “Aldo Moro” Bari Italy
4. Institute of Atmospheric Sciences and Climate (CNR‐ISAC) Padova Italy
Abstract
AbstractSeveral warm‐core cyclones in the Mediterranean, which were analyzed in the literature, are studied using ERA5 reanalysis, to identify the environment where they develop and distinguish tropical‐like cyclones from non‐tropical warm‐core cyclones. Initially, the cyclone phase space is analyzed to distinguish the cyclones that have a symmetrical deep warm core. Subsequently, the temporal evolution of several parameters is considered, including the distance between the area of maximum tangential wind speed and the cyclone center. Some differences are observed between the cyclones analyzed: one category of cyclones develops in areas of moderate‐low baroclinicity and intense convective processes, as occurs in tropical cyclones. Another group of cyclones develops in a strongly baroclinic environment with weak convective processes and intense vertical wind shear, as occurs in warm seclusions. Two cyclones, showing similarities with polar lows, are also identified.
Funder
Universidad de Castilla-La Mancha
Publisher
American Geophysical Union (AGU)
Cited by
2 articles.
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