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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 ...
Occurrence of Porphyra Vietnamensis (Bangiales, Rhodophyta) along the Goa Coast
(Indian Association for Limnology and Oceanography, 1981)
The occurrence of a red alga, Porphyra vietnamensis has been studied along the Goa Coast (west coast of India). The growth period was observed during the monsoon (July-October) and optimum growth was recorded during August, ...
Impact of temperature inversions on SST evolution in the South-Eastern Arabian Sea during the pre-summer monsoon season
(American Geophysical Union, 2004)
Temperature inversions are known to occur in the near-surface ocean regime where salinity stratification is large enough to influence the density field. However, they have not been known as features that alter near-surface ...
Enhanced biological production in the southeastern Arabian Sea during spring intermonsoon
(Italian Association of Oceanography and Limnology, 2012)
Hydrographic observations in the southeastern Arabian Sea (SEAS) have identified a warm (over 30 degrees C) and stratified water mass (stability more than 5x10 sup(-5) m sup(-1)) along the near shore area between 10 degrees ...
Hydrography and circulation in the western Bay of Bengal during the northeast monsoon
(American Geophysical Union, 1996)
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 seasonally reversing circulation. We ...
Quaternary radiolarian faunal changes in the tropical Indian Ocean: Inferences to paleomonsoonal oscillation of the 10 degrees S hydrographic front
(Current Science Association, Bangalore, 1997)
The northern Indian Ocean is characterized by three distinct surface water masses, i.e. (1) highly saline (greater than 34.5 ppt) Arabian Sea, (2) low saline (less than 34.5 ppt) Bay of Bengal and (3) a moderate salinity ...
Vertical distribution of temperature, salinity and density in the upper 500 metres of the north equatorial Indian Ocean during the north-east monsoon period
(National Institute of Sciences of India, 1968)
In the 4th and 5th scientific cruises of INS KISTNA under the Indian Programme of IIOE, five sections were worked out in the North Equatorial Indian Ocean during Jan-Feb 1963. Using the physical oceanographic data collected ...