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
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
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.