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V. V. S. S. Sarma

Researcher at National Institute of Oceanography, India

Publications -  67
Citations -  3774

V. V. S. S. Sarma is an academic researcher from National Institute of Oceanography, India. The author has contributed to research in topics: Bay & Monsoon. The author has an hindex of 34, co-authored 51 publications receiving 3220 citations. Previous affiliations of V. V. S. S. Sarma include Université Paul Cézanne Aix-Marseille III & Nagoya University.

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Increased marine production of N2O due to intensifying anoxia on the Indian continental shelf.

TL;DR: It is suggested that a global expansion of hypoxic zones may lead to an increase in marine production and emission of N2O, which, as a potent greenhouse gas, could contribute significantly to the accumulation of radiatively active trace gases in the atmosphere.
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A uniform, quality controlled Surface Ocean CO2 Atlas (SOCAT)

Benjamin Pfeil, +91 more
TL;DR: The surface ocean CO2 Atlas (SOCAT) project as discussed by the authors provides a publicly available, regularly updated, global data set of marine surface CO2, which had been subject to quality control (QC).
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An update to the Surface Ocean CO2 Atlas (SOCAT version 2)

Dorothee C. E. Bakker, +96 more
TL;DR: The Surface Ocean CO2 Atlas (SOCAT) as mentioned in this paper is an activity of the international marine carbon research community, providing access to synthesis and gridded fCO2 (fugacity of carbon dioxide) products for the surface oceans.
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Assessment of Godavari estuarine mangrove ecosystem through trace metal studies

TL;DR: Significant correlations observed between several couples of metals in different regions as well as between numbers of heavy metals with Total Suspended Matter in particulate organic matter could be an indication of the role of the complexation with organic matter in the distribution pattern of these metals.
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Physical forcing of biological productivity in the Northern Arabian Sea during the Northeast Monsoon

TL;DR: Time-series observations at a nominally fixed location in the northern Arabian Sea (21°N, 64°E) during the Northeast Monsoon (winter, February) of l997 showed the prevalence of cold sea-surface temperatures (SST) and deep mixed layers resulting from winter cooling and convection.