Abstract
Physical oceanography measurements reveal a strong salinity (0.18 psu km−1) and temperature (0.07 °C km−1) front off the east coast of India in December 1997. T–S diagrams suggest lateral mixing between the fresh water at the coast and the ambient warmer, saltier water. This front seems to be the result of southward advection of fresh and cool water, formed in the northern Bay of Bengal during the monsoon, by the East Indian Coastal Current, as suggested by the large-scale salinity structure in the SODA re-analysis and the anti-cyclonic gyre in the northwestern Bay of Bengal during winter. The data further reveals an offshore front in January, which appears to be the result of a meso-scale re-circulation around an eddy, bringing cold and freshwater from the northern Bay of Bengal further away from the shore. Our cruise data hence illustrates that very strong salinity fronts can appear in the Bay of Bengal after the monsoon, as a result of intense coastal circulation and stirring by eddies.
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References
Belkin IM, Cornillon PC, Sherman K (2009) Fronts in large marine ecosystems. Prog Oceanogr 81:223–236
Carton JA, Giese BS (2008) A re-analysis of ocean climate using simple ocean data assimilation (SODA). Mon Weather Rev 136:2999–3017
Chelton DB, Schlax MG, Samelson RM (2011) Global observations of nonlinear meso-scale eddies. Prog Oceanogr 91:167–216
Cushman-Roison B, Chassignet EP, Tang B (1990) Westward motion meso-scale eddies. J Phys Oceanogr 20:758–768
Ducet N, Le Traon PY (2000) Global high-resolution mapping of ocean circulation from TOPEX/Poseidon and ERS-1 and −2. J Geophys Res 105:19477–19498
Durand F, Shankar D, Birol F, Shenoi SSC (2009) Spatio temporal structure of the East India Coastal Current from satellite altimetry. J Geophys Res 114(C2)
Hareesh Kumar PV, Mohan Kumar N, Shyni TN, Raghunadha Rao A (2013) Observed variability of thermohaline fields, currents and eddies in the western Bay of Bengal during BOBMEX-99. Mar Geod 36:219–233. doi:10.1080/01490419. 2012.699505
Martin JM, Burton JD, Eisma D (eds) (1981) River inputs to ocean systems. United Nation Press, Geneva, 384
McCreary JP, Han W, Shankar D, Shetye SR (1996) Dynamics of the East India Coastal Current 2. Numerical solutions. J Geophys Res 101:13993–14010
Rao RR, Girish Kumar MS, Ravichandran M, Rao AR, Gopalakrishna VV, Thadathil P (2010) Inter-annual variability of Kelvin wave propagation in the wave guides of the equatorial Indian Ocean, the coastal Bay of Bengal and the southeastern Arabian Sea during 1993–2006. Deep-Sea Res I 57:1–13
Rintoul SR, Trull TW (2001) Seasonal evolution of the mixed layer in the sub Antarctic zone south of Australia. J Geophys Res 106:31447–31462
Saji NH, Goswami BN, Vinayachandran PN, Yamagata T (1999) A dipole mode in the tropical Indian Ocean. Nature 401:356–360
Schott F, Mc Creary JP (2001) The monsoon circulation of the Indian Ocean. Prog Oceanogr 51:1–123
Sengupta D, Bharath Raj GN, Shenoi SSC (2006) Surface freshwater discharge from Bay of Bengal runoff and Indonesian through flow in the tropical Indian Ocean. Geophys Res Lett. doi:10.1029/2006GL027573
Shankar D (2000) Seasonal cycle of sea level and currents along the coast of India. Curr Sci 78:279–288
Shankar D, Mc Creary JP, Han W, Shetye SR (1996) Dynamics of East India Coastal Current 1. Analytical solutions forced by interior Ekman pumping and local alongshore winds. J Geophys Res 101:13975–13991
Shenoi SSC (2010) Intra-seasonal variability of coastal currents around India: a review of the evidence from new observations. Indian J Geo-Mar Sci 39:489–496
Shenoi SSC, Shankar D, Shetye SR (2002) Differences in heat budgets of the near-surface Arabian Sea and Bay of Bengal: implications for the summer monsoon. J Geophys Res 107(C6)
Shetye SR, Shenoi SSC, Gouvela AD, Michael GS, Sundar D, Nampoothiri G (1991) Wind-driven coastal upwelling along the western boundary of the Bay of Bengal during the southwest monsoon. Cont Shelf Res 11:1397–1408
Shetye SR, Gouveia AD, Shankar D, Shenoi SSC, Vinayachandran PN, Sundar D, Michael GS, Nampoothiri G (1996) Hydrography and circulation in the western Bay of Bengal during the northeast monsoon. J Geophys Res 101:14011–14025
Sokolov S, Rintoul SR (2000) Structure of southern ocean fronts at 140°E. J Mar Syst 37:151–184
Sreenivas P, Gnanaseelan C, Prasad KVSR (2011) Influence of El Nino and Indian Ocean dipole on sea level variability in the Bay of Bengal. Glob Planet Chang. doi:10.1016/j.gloplacha,2011.11.001
Subramanian V (1993) Sediment load of Indian Rivers. Curr Sci 64:928–930
Suryanarayana A, Murthy VSN, Sarma YVB, Babu MT, Rao DP, Sastry JS (1992) Hydrographic features of the western Bay of Bengal in the upper 500m under the influence of northeast and southwest monsoons. In: Desai BN (ed) Oceanography of the Indian Ocean. IBH, New Delhi, pp 595–604
UNESCO (1988) River inputs into Ocean systems: status and recommendations for research. UNESCO Technical papers in marine science, No. 55, Final report of SCOR Working Group 46, Paris, 25 pp
Varkey MJ, Murty VSN, Suryanarayana A (1996) Physical oceanography of Bay of Bengal. Oceanography and marine biology: an annual review, vol 34. University College London Press, London, pp 1–70
Webster PJ, Moore AM, Loschnigg JP, Robert RL (1999) Coupled ocean–atmosphere dynamics in the Indian Ocean during 1997–98. Nature 401:356–360
Wu L, Wang F, Yuan D, Cui M (2007) Evolution of freshwater plumes and salinity fronts in the northern Bay of Bengal. J Geophys Res 112(C8)
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Authors are thankful to Shri. S. Ananthanarayanan, Director, NPOL, for the motivation and encouragement to carry out this study. The courteous efforts of the commanding officer, officers, and crew of INS Sagardhwani in smoothly conducting the mission are gratefully acknowledged.
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Hareesh Kumar, P.V., Mathew, B., Ramesh Kumar, M.R. et al. ‘Thermohaline front’ off the east coast of India and its generating mechanism. Ocean Dynamics 63, 1175–1180 (2013). https://doi.org/10.1007/s10236-013-0652-y
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DOI: https://doi.org/10.1007/s10236-013-0652-y