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Now showing items 11-20 of 22
Plankton of the Narmada Estuary and Adjacent Creeks
(Indian Association for Limnology and Oceanography, 1981)
Phytoplankton pigments and abundance of zooplankton in the Narmada Estuary, Bukki Creek and Dahej Creek were studied from March to September, 1979. The river sustained an appreciable quantity of phytoplankton pigments with ...
Assessment of water quality of a river-dominated estuary with hydrochemical parameters: A statistical approach.
(Springer, 2014)
This study was aimed (1) to evaluate the water quality of Chalakudy river, the fifth longest (145.5 km) river of Kerala (South India), by assessing the general hydrochemical parameters like temperature, dissolved oxygen ...
A sink for atmospheric carbon dioxide in the northeast Indian Ocean
(American Geophysical Union, 1996)
Intensive observations in the northeast Indian Ocean (Bay of Bengal) during the pre-southwest and northeast monsoon seasons 1991 reveal that freshwater discharge from rivers of the Indian subcontinent exerts the dominant ...
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 ...
Radiolarian monsoonal index Pyloniid group responds to astronomical forcing in the last approx. 500,000 y ears: Evidence from the Central Indian Ocean
(Indian Society for Prehistoric and Quaternary Studies, 1999)
Pyloniid radiolarians, oceanic micro-zooplanktons (surface water dwelling), are sensitive to monsoon sea surface temperature and salinity, and their variation down a core may provide an insight into the proxy climatic ...
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 ...
Postglacial Indian Ocean
(Elsevier, 2006)
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 ...
Hydrographic characterization of southeast Arabian Sea during the wane of southwest monsoon and spring intermonsoon
(Springer, 2008)
Seasonal variation of the hydrography along the southeast Arabian Sea is described using data collected onboard FORV Sagar Sampada in September-October 2003 (later phase of Southwest monsoon, SWM) and March-April 2004 ...
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 ...