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Influence of submonthly air–sea coupling on heavy precipitation events in the Western Mediterranean basin
Author(s) -
Berthou Ségolène,
Mailler Sylvain,
Drobinski Philippe,
Arsouze Thomas,
Bastin Sophie,
Béranger Karine,
Flaounas Emmanouil,
Lebeaupin Brossier Cindy,
Somot Samuel,
Stéfa Marc
Publication year - 2016
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.2717
Subject(s) - precipitation , climatology , mediterranean basin , mediterranean climate , environmental science , mediterranean sea , structural basin , water cycle , climate change , geography , oceanography , geology , meteorology , paleontology , ecology , archaeology , biology
Heavy precipitation events (HPEs) can be a major cause of damage and casualties in the Mediterranean basin. With the use of atmosphere–ocean coupled regional climate models (AORCMs) and the advantage of 24 years of simulation (1989–2012), we identified regions with potential impact of submonthly air–sea coupling on HPEs from among the regions hit by heavy rain during the Hydrological Cycle in the Mediterranean Experiment (HyMeX) first special observation period (SOP1): Valencia in Spain, the Cévennes in Southern France, Liguria in Northwestern Italy, Calabria in Southern Italy and Northeastern Italy. A first evaluation of the two AORCMs (MORCE and CNRM–RCSM4) against gridded precipitation datasets showed that 70–90% of the 30 most intense HPEs simulated were observed HPEs for most regions. The Cévennes, Valencia and Calabria were the only three regions to show a statistical relationship between rain differences and sea‐surface temperature (SST) differences where the low‐level jets that feed the events most frequently blow. This sensitivity of precipitation to SST changes is due to low‐level wind changes related to changes in surface heat fluxes. Based on the calculation of submonthly variations in these regions during HyMeX, HPEs on 28 September 2012 and 12 October 2012 in Valencia and on 25–26 October 2012 in the Cévennes have most probably been affected by submonthly air–sea coupling.