articleHydrography and circulation of the bay of Bengal during withdrawal phase of the southwest MonsoonHydrologie et circulation dans le golfe du Bengale à la renverse de la mousson du sud-ouest
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Cited by (14)
Paleoclimatic and paleoceanographic records from the Bay of Bengal sediments during the last 30 ka
2022, Journal of Asian Earth SciencesCitation Excerpt :The annual average SSS of the BoB ranges between 27 and 35 per mil (‰) (Roy, 2003). During ISM the salinity gradient becomes more extreme ranging from 21 to 35 ‰ due to increased precipitation (Sarma et al., 1999). Due to the combined effect of ISM and river influx, a low salinity of 24 ‰ forms in northern BoB during June and peaks in August whereas during May, highest salinity of 34 ‰ occurs in the BoB (Roy, 2003).
Assessing the effect of riverine discharge on planktic foraminifera: A case study from the marginal marine regions of the western Bay of Bengal
2021, Deep-Sea Research Part II: Topical Studies in OceanographyCitation Excerpt :The surface seawater pH is > 8 in the eastern Bay of Bengal and it decreases in the subsurface waters. The total alkalinity in the Bay of Bengal decreases with depth, varying from ~2100 μmol/kg to ~2450 μmol/kg and is strongly correlated to the ambient salinity and temperature (Sarma, 1998; Sarma et al., 1999). The dissolved inorganic carbon (DIC) shows a strong latitudinal trend in the western Bay of Bengal, varying from 2036 μmol/kg in the southwestern bay to 2034 μmol/kg in the northwestern bay during 1991, increasing to 2067 and 2198 μmol/kg, respectively, during 2011 (Sarma et al., 2015).
Extensive Accumulation of Nitrous Oxide in the Oxygen Minimum Zone in the Bay of Bengal
2023, Global Biogeochemical CyclesStatistical characteristics and thermohaline properties of mesoscale eddies in the Bay of Bengal
2021, Acta Oceanologica Sinica