Influence of environmental forcings on the seasonality of dissolved oxygen and nutrients in the Bay of Bengal

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ID: 294079
2007
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Abstract
Studies on seasonal variability of oxygen and nutrients during three seasons namely SW monsoon, fall intermonsoon and spring intermonsoon indicate influence of physical forcings on the distribution of these hydrochemical properties in the subsurface layer. In the open ocean the Minimum Oxygen Layer (MOL 10mu Mol L-1) during the southwest monsoon and fall intermonsoon is mostly confined to the north of 11N due to the penetration of high salinity water in the deeper waters of the central Bay. During spring intermonsoon MOL is mostly confined to the northern region between 14 to 20N with a narrow band of suboxic waters ( 5mu Mol L-1) around 19 to 20N. Along the western margin, the MOL occupies a larger area in the intermediate and deeper waters during the SW monsoon and fall intermonsoon with a thick layer of suboxic waters during the SW monsoon which gets reduced and confined to the northern region during fall intermonsoon. The core of suboxic waters seems to disappear during the spring intermonsoon. The displacement of the water mass to shallower depths under the influence of cold core eddies
Reference Key
openalex_W2243395629 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors S. Sardessai, N. Ramaiah, S. Prasanna Kumar, S. N. De Sousa
Journal journal of marine research
Year 2007
DOI
10.1357/002224007780882578
URL
https://doi.org/10.1357/002224007780882578
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