User profiles for D. Shankar

D Shankar

National Institute of Oceanography
Verified email at nio.org
Cited by 6803

The monsoon currents in the north Indian Ocean

D Shankar, PN Vinayachandran… - Progress in …, 2002 - Elsevier
The monsoon currents are the seasonally reversing, open-ocean currents that flow between
the Arabian Sea and the Bay of Bengal, the two wings of the north Indian Ocean. The …

Hydrography and circulation in the western Bay of Bengal during the northeast monsoon

SR Shetye, AD Gouveia, D Shankar… - Journal of …, 1996 - Wiley Online Library
The Bay of Bengal, a semienclosed tropical basin that comes under the influence of monsoonal
wind and freshwater influx, is distinguished by a strongly stratified surface layer and a …

[HTML][HTML] India and its pluralistic health system–a new philosophy for Universal Health Coverage

…, J Porter, GKG Pillai, L Abraham, D Shankar… - The Lancet Regional …, 2023 - thelancet.com
In this article we attempt to put forth insights into using traditional medicine (TM) systems to
achieve Universal Health Coverage (UHC). We discuss the need for reimagining India's …

Differences in heat budgets of the near‐surface Arabian Sea and Bay of Bengal: Implications for the summer monsoon

SSC Shenoi, D Shankar… - Journal of Geophysical …, 2002 - Wiley Online Library
An analysis of the heat budgets of the near‐surface Arabian Sea and Bay of Bengal shows
significant differences between them during the summer monsoon (June–September). In the …

Are sea-level-rise trends along the coasts of the north Indian Ocean consistent with global estimates?

AS Unnikrishnan, D Shankar - Global and Planetary Change, 2007 - Elsevier
Mean-sea-level data from coastal tide gauges in the north Indian Ocean were used to show
that low-frequency variability is consistent among the stations in the basin. Statistically …

On the dynamics of the Lakshadweep high and low in the southeastern Arabian Sea

D Shankar, SR Shetye - Journal of Geophysical Research …, 1997 - Wiley Online Library
Hydrography and altimetry show that a ”high” in surface topography forms off southwest India
in January (midnortheast monsoon) and that a ”low” forms during the southwest monsoon; …

Dynamics of the east India coastal current: 2. Numerical solutions

JP McCreary, W Han, D Shankar… - Journal of Geophysical …, 1996 - Wiley Online Library
A linear, continuously stratified model is used to investigate the dynamics of the East India
Coastal Current (EICC). Solutions are found numerically in a basin that resembles the Indian …

Basin‐wide seasonal evolution of the Indian Ocean's phytoplankton blooms

M Lévy, D Shankar, JM André… - Journal of …, 2007 - Wiley Online Library
A climatology of Sea‐viewing Wide Field‐of‐View Sensor (SeaWiFS) chlorophyll data over
the Indian Ocean is used to examine the bloom variability patterns, identifying spatio‐…

Dynamics of the East India Coastal Current: 1. Analytic solutions forced by interior Ekman pumping and local alongshore winds

D Shankar, JP McCreary, W Han… - Journal of Geophysical …, 1996 - Wiley Online Library
… In the southern Bay, regions of positive d driven by negative œ also appear in the eastern …
d in the southern Bay, •,nd by May the region of positive d exists only in a band of increased d

[PDF][PDF] The role of CREB as a proto-oncogene in hematopoiesis and in acute myeloid leukemia

DB Shankar, JC Cheng, K Kinjo, N Federman… - Cancer cell, 2005 - cell.com
… alive without relapse or persistent disease was lower in those patients overD: FISH on … d:
K562 cells were transfected with TKO reagent alone, 100 nM luciferase siRNA, or 100 nM 3# …