Search
Now showing items 1-10 of 30
BOBMEX: The Bay of Bengal Monsoon Experiment
(American Meteorological Society, 2001)
The first observational experiment under the Indian Climate Research Programme, called the Bay of Bengal Monsoon Experiment (BOBMEX), was carried out during July-August 1999. BOBMEX was aimed at measurements of important ...
Warm pool thermodynamics from the Arabian Sea Monsoon Experiment (ARMEX)
(American Geophysical Union, 2008)
Before the onset of the south Asian summer monsoon, sea surface temperature (SST) of the north Indian Ocean warms to 30-32 degrees C. Climatological mean mixed layer depth in spring (March-May) is 10-20 m, and net surface ...
Seasonal variability of cyclone heat potential in the Bay of Bengal
(Kluwer Academic, 2004)
Monthly maps of cyclone heat potential (CHP) in the Bay of Bengal have been prepared by using Levitus climatological data set. Seasonal variability of CHP in the Bay of Bengal has been studied using the CTD data sets ...
Mean surface fields of heat budget components over the warm pool in the Bay of Bengal during post-monsoon season
(Tata McGraw-Hill, New Delhi, India, 1999)
Surface meteorological data collected onboard research vessels ORV Sagarkanya and Gaveshani during 1983-85 have been used in these studies. The analysis revealed that the Mean Sea surface temperature (SST was greater than ...
Influence of the monsoon trough on air-sea interaction in the head of the Bay of Bengal during the southwest monsoon of 1990 (monsoon trough boundary layer experiment - 90)
(Kluwer, 1997)
The analysis of 3-hourly time-series data on surface meteorological parameters collected at 20 degrees N, 89 degrees E in the head of the Bay of Bengal during the southwest monsoon period (18 August - 19 Spetember) of 1990 ...
Surface temperature pattern of the Indian Ocean before summer monsoon
(Indian Association for Limnology and Oceanography, 1985)
The surface meteorological data collected during 1963 and 1964 indicate that the northward migration of the ITCZ is associated with a shift of the warm waters to the northern Indian Ocean. The warmer waters, found in the ...
Past 100 Ky surface salinity-gradient response in the eastern Arabian Sea to the summer monsoon variation recorded by delta super(18)O of G. sacculifer
(Elsevier, 2005)
Northward flowing coastal currents along the western margin of India during winter-spring advect low-salinity Bay of Bengal water in to the Eastern Arabian Sea producing a distinct low-salinity tongue, the strength of which ...
Is an onset vortex important for monsoon onset over Kerala?
(Springer, 2012)
Inter-annual variability in the formation of the mini warm pool [sea-surface temperature (SST) more than 30 degrees C] over the south eastern Arabian Sea (SEAS) and its role in the formation of the monsoon onset vortex ...
Radiolarian fluxes from the southern Bay of Bengal: sediment trap results
(Pergamon, 2002)
A study of radiolarian fluxes collected during 1991-93 from time-series sediment traps deployed at 1071 and 3010 m water depth in the southern Bay of Bengal (SBBT) yielded 40 species/groups of radiolarians. Among the order ...
Seasonal sea surface temperature contrast between the Holocene and last glacial period in the western Arabian Sea (Ocean Drilling Project Site 723A): Modulated by monsoon upwelling
(AGU, 2005)
Annual, summer, and winter sea surface temperatures (SSTs) in the western Arabian Sea were reconstructed through the last 22 kyr using artificial neural networks (ANNs) based on quantitative analyses of planktic foraminifera. ...