6533b853fe1ef96bd12ac3a3

RESEARCH PRODUCT

West African Monsoon influence on the summer Euro-Atlantic circulation

Marco GaetaniBernard FontaineHervé DouvilleBenjamin Pohl

subject

Convection010504 meteorology & atmospheric sciencesAtmospheric circulation[SDE.MCG]Environmental Sciences/Global ChangesSubsidence (atmosphere)010502 geochemistry & geophysicsMonsoon01 natural sciencesWest african[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsCirculation (fluid dynamics)13. Climate actionNorth Atlantic oscillation[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyGeneral Earth and Planetary SciencesClimate model[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyGeology0105 earth and related environmental sciences

description

International audience; The West African Monsoon (WAM) influence on the interannual variability of the summer atmospheric circulation over North Atlantic and Europe is investigated over the period 1971-2000. A set of sensitivity experiments performed through the Arpege-Climat atmospheric general circulation model is analyzed, using the so-called "grid-point nudging" technique, where the simulated atmospheric fields in the WAM region are relaxed towards the ERA40 reanalysis. Observations confirm that a sizable part of the Euro-Atlantic circulation variability is related to the WAM, with anomalies of reinforced convection in the Sudan-Sahel region associated with positive North Atlantic Oscillation (NAO) phases and subsidence over eastern Mediterranean. The nudged simulations highlights the role of the WAM in driving the mid-latitudes circulation. A strong monsoon is related to high-pressure anomalies over the Azores and positive NAO phases.

10.1029/2011gl047150https://hal.archives-ouvertes.fr/hal-00582619/document