On the possible mechanisms of the evolution of a mini-warm pool during thepre-summer monsoon season and the genesis of onset vortex in the south-eastern Arabian Sea

Citation
Rr. Rao et R. Sivakumar, On the possible mechanisms of the evolution of a mini-warm pool during thepre-summer monsoon season and the genesis of onset vortex in the south-eastern Arabian Sea, Q J R METEO, 125(555), 1999, pp. 787-809
Citations number
74
Categorie Soggetti
Earth Sciences
Journal title
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
ISSN journal
00359009 → ACNP
Volume
125
Issue
555
Year of publication
1999
Part
A
Pages
787 - 809
Database
ISI
SICI code
0035-9009(199904)125:555<787:OTPMOT>2.0.ZU;2-L
Abstract
During the pre-summer monsoon season (February-May), the near-surface water s in the Arabian Sea progressively warm up and a mini-warm pool with a core >30 degrees C is manifested in the south-eastern region. The possible mech anisms for the observed seasonal build-up of this mini-warm pool are examin ed, utilizing all the available monthly mean climatologies of surface wind field, surface heat fluxes, near-surface thermohaline fields, near-surface circulation, and mean sea level as monitored by satellites and by some of t he recent model solutions on the Arabian Sea circulation. During winter (November-February), the equatorward-flowing East India Coast al Current in the western Bay of Bengal and westward-flowing North Equatori al Current in the southern Bay bring low-saline waters into the south-easte rn Arabian Sea, causing a haline stratification within the near-surface iso thermal layer. During December-April, the positive surface-wind-stress curl and the associated Ekman divergence shoals the pycnocline. A south-westwar d propagating mode-2 Rossby wave from off south-west India seen in satellit e-derived mean sea level and model solutions also modulates the underlying pycnocline. During the pre-summer monsoon season, under clear skies and lig ht wind conditions, the radiative heat input overwhelms turbulent heat loss es at the air-sea interface, and the net surplus heat energy is absorbed in a shallow haline stratified near-surface layer, resulting in the formation of the observed mini-warm pool. An examination of historical data on the genesis of monsoon onset vortices reveals that on most occasions the genesis has occurred over this mini-warm pool region. Evidence for the geographic coincidence in the occurrence of the genesis of onset vortex and the sea surface temperature maxima during i ndividual years of a three decade period (1961-90) is presented.