Vinayachandran P. N. auteur aut IRD Shankar D. auteur aut IRD Kurian J. auteur aut IRD Durand Fabien auteur aut IRD Shenoi S. S. C. auteur aut IRD text journalArticle eng text/pdf born digital access Warm pools - regions with sea surface temperature (SST) in excess of 28 degrees C - in the ocean occupy a special place in tropical climate owing to their impact on tropical convection. The southeastern Arabian Sea presents SST in excess of 30 degrees C for two to three months preceding the onset of the summer (southwest) monsoon over India. Recently, several attempts have been made to understand the processes that cause such high SSTs in the region. The literature is also strewn with observations and modelling of a 'monsoon onset vortex' forming over the warm pool. This paper is a review of our current understanding of the Arabian Sea mini warm pool and its possible role in the formation of the monsoon onset vortex. specialized arabian Sea mini warm pool monsoon onset vortex INDE OCEAN INDIEN 032 021 93 2 203-214 2007 0011-3891 https://www.documentation.ird.fr/hor/PAR00002040 0011-3891 [F B010093145] https://www.documentation.ird.fr/hor/PAR00002040 https://www.documentation.ird.fr/intranet/publi/2025-02/010093145.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2007-12-21 2025-02-28 PAR00002040 fre