Results 251 to 260 of about 113,932 (305)
Linking Biological Parameters to Fishery Management: Stock Assessment of Green Tiger Prawn, <i>Penaeus semisulcatus</i> De Haan, 1844 Along the Red Sea Coast of Saudi Arabia. [PDF]
Biology (Basel)Tıraşın EM +8 more
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Nature Reviews Earth & Environment, 2021
An article in Climate Dynamics documents tropical cyclone characteristics in the northern Indian Ocean, revealing marked changes in the Arabian Sea.
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An article in Climate Dynamics documents tropical cyclone characteristics in the northern Indian Ocean, revealing marked changes in the Arabian Sea.
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2020
The Arabian Sea makes contributions to global biogeochemical cycles that are far in excess of what might be expected from its modest size. It experiences extremes in atmospheric forcing, asymmetrically distributed over the region, that brings about exceptionally large hydrographical changes and produce a wide variety of ecosystems or biogeochemical ...
Naqvi, S.W.A., Naik, H., Narvekar, P.V.
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The Arabian Sea makes contributions to global biogeochemical cycles that are far in excess of what might be expected from its modest size. It experiences extremes in atmospheric forcing, asymmetrically distributed over the region, that brings about exceptionally large hydrographical changes and produce a wide variety of ecosystems or biogeochemical ...
Naqvi, S.W.A., Naik, H., Narvekar, P.V.
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Intensified Arabian Sea tropical storms
Nature, 2012Arising from A. T. Evan, J. P. Kossin, C. E. Chung & V. Ramanathan , 94–97 (2011)10.1038/nature10552 Tropical cyclones over the Arabian Sea in the pre-monsoon season (May–June) have intensified since 1997 (ref. 1, Fig. 1a) owing to significant reductions in storm-ambient vertical wind shear (VWS) in
Bin, Wang, Shibin, Xu, Liguang, Wu
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1973
When the IIOE was planned, it was considered a valuable objective to examine the upwelling regions which had been reported in the Arabian Sea (Bobzin, 1922) but had never before been the object of scientific observation.
R. I. Currie +2 more
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When the IIOE was planned, it was considered a valuable objective to examine the upwelling regions which had been reported in the Arabian Sea (Bobzin, 1922) but had never before been the object of scientific observation.
R. I. Currie +2 more
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1997
Abstract : The long-term goal of this research is to identify and understand the mechanisms that determine the features of stratification and motion in the upper 200 meters of mid-latitude oceans. This is the depth range over which surface fluxes of momentum and buoyancy have direct influence.
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Abstract : The long-term goal of this research is to identify and understand the mechanisms that determine the features of stratification and motion in the upper 200 meters of mid-latitude oceans. This is the depth range over which surface fluxes of momentum and buoyancy have direct influence.
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Denitrification in the Arabian Sea
Deep Sea Research Part A. Oceanographic Research Papers, 1982Abstract Estimates of the amount of denitrification in the Arabian Sea are inconsistent, and so two methods of calculation of ‘original’ nitrate concentrations used in earlier studies have been reviewed. Nitrite at intermediate depths was not restricted to the Persian Gulf water; concentrations were maximal much shallower than the depths of the ...
S.Wajih A. Naqvi +2 more
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Understanding the Arabian Sea: Reflections on the 1994–1996 Arabian Sea Expedition
Deep Sea Research Part II: Topical Studies in Oceanography, 2001Abstract The Arabian Sea Expedition, now five years past its field observations, is at a stage when some of its dominant themes can be summarized. Of the large range of possible topics, five are considered here: (1) Is the Arabian Sea a source or sink for carbon dioxide?; (2) Is the Arabian Sea Mother Nature's iron experiment?; (3) Do grazing ...
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Nature, 1990
Sir-Variations in the oxigen isotope content (δ^(18)O) of planktonic foraminifera from the Arabian Sea have been cited as evidence for stronger northeast monsoon current at the last glacial maximum (LGM), about 18 kyr ago, than during the present day.
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Sir-Variations in the oxigen isotope content (δ^(18)O) of planktonic foraminifera from the Arabian Sea have been cited as evidence for stronger northeast monsoon current at the last glacial maximum (LGM), about 18 kyr ago, than during the present day.
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