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Gobiiform Fishes of the Arabian Sea
2021Gobiiform fishes are a highly diverse group with global distribution. In the Arabian Sea, this group is represented by four families—Butidae, Eleotridae, Gobiidae, and Oxudercidae—comprising 215 species in 77 genera. There are no endemic species within the Butidae.
Zeehan Jaafar +1 more
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Chaetognaths of the Arabian Sea
1973During the IIOE (1959–1965) the Indian Ocean Biological Centre (IOBC) received 1927 Zooplankton samples, of which 1548 are standard ones (IOBC, 1969). Of these, 614 samples belong to the area extending from 10° S to 25° N lat. between 20° E and 80° E long. The chaetognaths identified from these 614 samples form the basis of the present study.
V. R. Nair, T. S. S. Rao
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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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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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Mesopelagic microplankton of the Arabian Sea
Deep Sea Research Part I: Oceanographic Research Papers, 2003Abstract The Arabian Sea is notable for its dramatic monsoonal effects on euphotic zone biogeochemical processes and the large spatial extent of its mesopelagic oxygen minimum zone. As part of the US Joint Global Ocean Flux Study Arabian Sea project, we sampled microplankton (organisms 20–200 μm including diatoms, dinoflagellates, ciliates ...
Gowing, Marcia M. +3 more
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Reefs and Coral Communities of the Arabian Gulf and Arabian Sea
2000Abstract The seas included in this chapter are the Arabian or Persian Gulf (simply “the Gulf “ in local usage), several of its components which experience extreme environmental characteristics, as well as the Gulf of Oman, Arabian Sea and Gulf of Aden (Fig. 9.1). These are all marginal seas of the Indian Ocean, partly because of latitude,
C R C Sheppard +3 more
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Nitrous oxide in the Arabian Sea
Deep Sea Research Part A. Oceanographic Research Papers, 1991Abstract Measurements of nitrous oxide (N 2 O) at 16 stations in the Arabian Sea reveal high degrees of surface saturation (186 ± 37%) and consequently large atmospheric fluxes of N 2 O (4.46 ± 2.60 μ mol m −2 day −1 ). Unusually high for a non-upweling period, these values reflect the large vertical gradients of N 2 O just below the mixed layer as
Naqvi, S.W.A., Noronha, R.J.
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Surficial sediments of the Arabian Sea
Marine Geology, 1981Abstract Coarse-grained, low-carbonate sediments with high abundances of quartz and feldspar in the northerly areas of the Arabian Sea close to land reflect significant terrigenous sediment in fluxes primarily from the Indus River, and to some extent, from other sources.
Venkatarathnam Kolla +2 more
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On the heat budget of the Arabian Sea
Deep Sea Research Part I: Oceanographic Research Papers, 2009Abstract This study analyzes the heat budget of the Arabian Sea using satellite-derived sea-surface temperature (SST) from 1985 to 1995 along with other data sets. For a better understanding of air–sea interaction, canonical average monthly fields representing the spatial and temporal structure of the various components of the heat balance of the ...
Deanna Wilson-Diaz +2 more
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2009
Vasco da Gama left Malindi for Calicut on 24 April 1498 and the fleet arrived near Calicut, India on 20 May 1498. The king of Calicut sent men to Pandarane, in order to conduct the Captain major to where the king awaited him. The king of Portugal D. Manuel, had ordered the three ships built, and had appointed Vasco da Gama and instructed him not to ...
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Vasco da Gama left Malindi for Calicut on 24 April 1498 and the fleet arrived near Calicut, India on 20 May 1498. The king of Calicut sent men to Pandarane, in order to conduct the Captain major to where the king awaited him. The king of Portugal D. Manuel, had ordered the three ships built, and had appointed Vasco da Gama and instructed him not to ...
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