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Now showing items 21-30 of 114
Thermal response of upper layers of Bay of Bengal to forcing of a severe cyclonic storm: A case study
(NISCAIR, New Delhi, 1993)
Upper ocean response to forcing of a severe cyclonic storm during May 1990 in the western Bay of Bengal was studied using the XBT data sets collected (4 d after passage of storm) under Indian TOGA programme. A maximum ...
On the warm pool dynamics in the southeastern Arabian Sea during April – May 2005 based on the satellite remote sensing and ARGO float data
(Society of Photo-Optical Instrumentation Engineers, 2006)
Observational data from the Arabian Sea Monsoon Experiment (ARMEX-Phase IIA) in the southeastern Arabian Sea (SEAS) showed intense warming with the SST up to 31.5°C during April – May 2005. Analysis of 5–day repeat cycles ...
An intrathermocline eddy and a tropical cyclone in the Bay of Bengal
(Nature Publishing Group, 2017)
The Bay of Bengal, subjected to monsoonal forcing and tropical cyclones, displays a complex field of ocean eddies. On 5 December 2013 a sub-surface vortex or Intrathermocline Eddy (ITE) composed of water characteristic of ...
Marine boundary layer characteristics during a cyclonic storm over the Bay of Bengal
(Indian Academy of Sciences, 2006)
During the period 12–16 June 1996 a tropical cyclonic storm formed over the southwest Bay of Bengal and moved in a north–northeasterly direction. The thermodynamic characteristics of this system are investigated by utilizing ...
Low frequency variability of the Indian Ocean from TOPEX/POSEIDON sea surface height anomalies
(NIO, Dona Paula, Goa (India), 2000)
The sea surface height (SSH) anomalies derived from TOPEX/POSEIDON altimeter have been utilized to study the variability of surface circulation in the Indian Ocean during 1993-1999. The Western Bay, southeastern Arabian ...
Internal waves over the shelf in the western Bay of Bengal: A case study
(Springer, 2017)
Generation and propagation of internal waves (IWs) in the coastal waters of the extended shelf of the western Bay of Bengal are investigated for late winter by using the Massachusetts Institute of Technology General ...
Seasonal variability in the vertical current structure and kinetic energy in the Central Indian Ocean Basin
(Pergamon, 2001)
Seasonal variability in the currents at the subsurface (450-670 m), intermediate (1150-1370 m), deeper (3450-3670 m) and near-bottom (4270-5100 m) depths at three mooring station in the Central Indian Ocean Basin (CIOB) ...
Monsoonal reversal of remote sensing biases in latent heat flux over eastern Arabian Sea
(American Geophysical Union, 2006)
The Arabian Sea is a unique basin where a number of atmospheric and oceanographic processes occur due to the contrasting climatic conditions, which it experiences. The drastic monsoonal variability occurring in the boundary ...
T-S variability and volume transport in the central Bay of Bengal during southwest monsoon
(NISCAIR, CSIR, 1996)
The variability of temperature and salinity along 11 degrees N and 12 degrees N sections in the Bay of Bengal during southwest monsoon months (July-September) was found to be large in the upper 200 m west of 83 degrees E ...
On the circulation in the Bay of Bengal during northern spring inter-monsoon (March-April 1987)
(Elsevier, 2003)
Temperature and salinity data collected from the Bay of Bengal 22 March-28 April 1987 (Northern spring inter-monsoon) identified the seasonal anticyclonic gyre (ACG) at 16 degrees N, 86 degrees E characterized by warm ...