Premium
A 40‐year climatological study of relative vorticity distribution over the Mediterranean
Author(s) -
Flocas H.A.,
Maheras P.,
Karacostas T.S.,
Patrikas I.,
Anagnostopoulou C.
Publication year - 2001
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.705
Subject(s) - climatology , vorticity , positive vorticity advection , potential vorticity , mediterranean climate , geostrophic wind , cyclogenesis , mediterranean sea , cyclone (programming language) , spatial distribution , environmental science , geology , synoptic scale meteorology , atmospheric sciences , oceanography , geography , meteorology , vortex , remote sensing , archaeology , field programmable gate array , computer hardware , computer science
A climatological study of the spatial and temporal distribution of mean relative geostrophic vorticity over the Mediterranean region is examined for a period of 40 years (1958–1997). Two major cyclonic vorticity maxima are found in the Mediterranean at low levels, one covers the Gulf of Genoa and south Italy and the second is located over the southeastern Aegean Sea with different diurnal and seasonal characteristics, controlling cyclone formation. At upper levels, a large scale cyclonic vorticity zone covers the whole Mediterranean region with notably increased values at 300 hPa, being associated with jet stream dynamics, especially in the eastern Mediterranean. The seasonal changes of the horizontal vorticity distribution substantially reduce with height while the diurnal changes become unimportant at upper levels. Furthermore, the investigation of the vertical vorticity structure separately for the main cyclonic centres in the Mediterranean implies the different mechanisms that are responsible for cyclone formation in the western and eastern basin. Copyright © 2001 Royal Meteorological Society