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Distinctive phytoplankton size responses to the nutrient enrichment of coastal upwelling and winter convection in the eastern Arabian Sea
Even though the seasonal pattern of phytoplankton biomass distribution in the seas around
India is reasonably well understood, there is relatively little information on phytoplankton …
India is reasonably well understood, there is relatively little information on phytoplankton …
Dynamics of A ndaman S ea circulation and its role in connecting the equatorial I ndian O cean to the B ay of B engal
Circulation in the Bay of Bengal (BoB) is driven not only by local winds, but are also strongly
forced by the reflection of equatorial Kelvin waves (EKWs) from the eastern boundary of the …
forced by the reflection of equatorial Kelvin waves (EKWs) from the eastern boundary of the …
Influence of El Niño and Indian Ocean Dipole on sea level variability in the Bay of Bengal
Zonally oscillating seasonal equatorial winds generate pairs of upwelling and downwelling
Kelvin waves in the Equatorial Indian Ocean, which then advance in to the coastal Bay of …
Kelvin waves in the Equatorial Indian Ocean, which then advance in to the coastal Bay of …
Unprecedented surface chlorophyll blooms in the southeastern Arabian Sea during an extreme negative Indian Ocean Dipole
Observations of ocean color in the southeastern Arabian Sea (SEAS) during the late boreal
summer and fall of 2016 reveal the highest surface chlorophyll concentrations (> 1.0 mg m …
summer and fall of 2016 reveal the highest surface chlorophyll concentrations (> 1.0 mg m …
Intraseasonal response of the northern Indian Ocean coastal waveguide to the Madden‐Julian Oscillation
J Vialard, SSC Shenoi, JP Mccreary… - Geophysical …, 2009 - Wiley Online Library
A new observational record of upper‐ocean currents at 15° N on the western coast of India
is dominated by intraseasonal (55–110 day) variations of alongshore currents, whereas sea …
is dominated by intraseasonal (55–110 day) variations of alongshore currents, whereas sea …
Inhibition of mixed-layer deepening during winter in the northeastern Arabian Sea by the West India Coastal Current
Though the deep mixed layers (MLs) that form in the northeastern Arabian Sea (NEAS)
during the winter monsoon (November–February) have been attributed to convective mixing …
during the winter monsoon (November–February) have been attributed to convective mixing …
Role of physical processes in determining the nature of fisheries in the eastern Arabian Sea
We use available data and model simulations to make a case for physical forcing of the
spatial variation in the nature of fisheries off the west coast of India in the eastern Arabian …
spatial variation in the nature of fisheries off the west coast of India in the eastern Arabian …
Observed intraseasonal and seasonal variability of the West India Coastal Current on the continental slope
We present current data from acoustic Doppler current profilers (ADCPs) moored on the
continental slope off the west coast of India. The data were collected at four locations …
continental slope off the west coast of India. The data were collected at four locations …
Origins of wind‐driven intraseasonal sea level variations in the North Indian Ocean coastal waveguide
In this paper, we show that a linear, continuously stratified ocean model reproduces
observed wind‐driven intraseasonal sea level variability in the coastal waveguide of the …
observed wind‐driven intraseasonal sea level variability in the coastal waveguide of the …
Consequences of inhibition of mixed‐layer deepening by the West India Coastal Current for winter phytoplankton bloom in the northeastern Arabian Sea
The intense winter phytoplankton bloom during November–February in the northeastern
Arabian Sea (NEAS) was thought, until recently, to be controlled only by a convective …
Arabian Sea (NEAS) was thought, until recently, to be controlled only by a convective …