2022
DOI: 10.1016/j.dsr.2022.103770
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Freshwater transport by eddies within the Bay of Bengal's central axis

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Cited by 4 publications
(3 citation statements)
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“…Nonetheless, circulation reverses semi-annually, although not exactly matching wind direction, and in both seasons circulation is largely unorganised and characterised by meso-scale cyclonic (during the northeast monsoon) and anti-cyclonic (January to April) eddies (Chamarthi et al, 2008;Brewer et al, 2015;Behara and Vinayachandran, 2016;Rainville et al, 2022). Because the BoB receives a vast volume of freshwater on a seasonal time scale this water needs to be transported out of the bay (Behara and Vinayachandran, 2016;Herron et al, 2022). This is achieved largely by the East Indian Coastal Current (EICC) on the western side of the bay during November-January and by equator-ward flowing currents on the eastern side during both summer and winter (Chaitanya et al, 2014;Behara and Vinayachandran, 2016 and references therein, although not all studies agree on this e.g., Rainville et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…Nonetheless, circulation reverses semi-annually, although not exactly matching wind direction, and in both seasons circulation is largely unorganised and characterised by meso-scale cyclonic (during the northeast monsoon) and anti-cyclonic (January to April) eddies (Chamarthi et al, 2008;Brewer et al, 2015;Behara and Vinayachandran, 2016;Rainville et al, 2022). Because the BoB receives a vast volume of freshwater on a seasonal time scale this water needs to be transported out of the bay (Behara and Vinayachandran, 2016;Herron et al, 2022). This is achieved largely by the East Indian Coastal Current (EICC) on the western side of the bay during November-January and by equator-ward flowing currents on the eastern side during both summer and winter (Chaitanya et al, 2014;Behara and Vinayachandran, 2016 and references therein, although not all studies agree on this e.g., Rainville et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…Herron et al (2022) pointed out that mesoscale eddies could drive surface freshwater from the northern BoB southward into the southern BoB, and freshwater flux in the southern BoB usually reaches its delayed peak in summer. Influenced by surface freshwater, mesoscale eddies in the BoB have a relatively complex vertical thermohaline structure with seasonal variations (Cui et al, 2022), and their transport of water mass is expected to play a significant role in the redistribution of surface freshwater (Cui et al, 2022;Herron et al, 2022;Mahadevan et al, 2016;Paul et al, 2021). On the other hand, Zhu et al (2022) revealed that in November 2016, the EICC transported low-salinity water from the northern BoB southward to east of Sri Lanka, and meanwhile, a cyclonic eddy developed east of Sri Lanka, moving southwestward and transporting the low-salinity water to the southern AS.…”
mentioning
confidence: 99%
“…In the northern BoB, with an excess of freshwater input, surface freshwater flux reaches its maximum in winter due to freshwater accumulation at the end of the wet summer monsoon season. Herron et al (2022) pointed out that mesoscale eddies could drive surface freshwater from the northern BoB southward into the southern BoB, and freshwater flux in the southern BoB usually reaches its delayed peak in summer. Influenced by surface freshwater, mesoscale eddies in the BoB have a relatively complex vertical thermohaline structure with seasonal variations (Cui et al, 2022), and their transport of water mass is expected to play a significant role in the redistribution of surface freshwater (Cui et al, 2022;Herron et al, 2022;Mahadevan et al, 2016;Paul et al, 2021).…”
mentioning
confidence: 99%