Abstract
The present study investigates the mixed layer variations near mesoscale eddies in the Bay of Bengal (BoB) using satellite altimeter and Argo data. Furthermore, the factors responsible for sea surface variations near mesoscale eddies are analyzed using the mixed layer heat and salinity budgets estimated from Argo profiles. In the diagnostic mixed layer heat budget analysis, the entrainment term is parametrized based on the presence and absence of the barrier layer. The role of inversion and barrier layers on eddy-induced temperature variations is also examined near eddy locations. Results showed that anti-cyclonic eddies deepen mixed layer depth (MLD) and barrier layer thickness (BLT). Whereas, near cyclonic eddies shallower MLD and BLT is evident. However, MLD and BLT variations near mesoscale eddies are prominent during monsoon and winter seasons, respectively. Heat budget analysis near eddy locations depicts that surface heat fluxes and vertical entrainment are the primary factors responsible for temperature variations near mesoscale eddies. Similarly, the salinity budget analysis near eddy locations reveals that horizontal advection (stirring effect) is the predominant processes responsible for the salinity variations. The outcome of the present study is believed to be useful in validating and improving the eddy-resolving ocean models.
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References
Agarwal N, Sharma R, Parekh A, Basu S, Sarkar A, Agarwal VK (2012) Argo observations of barrier layer in the tropical Indian Ocean. Adv Space Res 50(5):642–654. https://doi.org/10.1016/j.asr.2012.05.021
Akhil VP, Durand F, Lengaigne M, Vialard J, Keerthi MG, Gopalakrishna VV, de Boyer Montégut C (2014) A modeling study of the processes of surface salinity seasonal cycle in the Bay of Bengal. J Geophys Research: Oceans 119(6):3926–3947. https://doi.org/10.1002/2013JC009632
Babu KN, Sharma R, Agarwal N, Agarwal VK, Weller RA (2004) Study of the mixed layer depth variations within the north Indian Ocean using a 1-D model. J Geophys Research: Oceans 109(C8). https://doi.org/10.1029/2003JC002024
Balaguru K, Chang P, Saravanan R, Leung LR, Xu Z, Li M, Hsieh JS (2012) Ocean barrier layers’ effect on tropical cyclone intensification. Proc Natl Acad Sci 109(36):14343–14347. https://doi.org/10.1073/pnas.1201364109
Bhat GS, Gadgil S, Kumar PH, Kalsi SR, Madhusoodanan P, Murty VSN, Vinayachandran PN (2001) BOBMEX: the Bay of Bengal monsoon experiment. Bull Am Meteorol Soc 82(10):2217–2244. https://doi.org/10.1175/1520-0477(2001)082<2217:BTBOBM>2.3.CO;2
Bindoff NL, Mcdougall TJ (1994) Diagnosing climate change and ocean ventilation using hydrographic data. J Phys Oceanogr 24(6):1137–1152. https://doi.org/10.1175/1520-0485(1994)024%3C1137:DCCAOV%3E2.0.CO;2
Buckley JM, Mingels B, Tandon A (2020) The impact of lateral advection on SST and SSS in the northern Bay of Bengal during 2015. Deep Sea Res Part II 172:104653. https://doi.org/10.1016/j.dsr2.2019.104653
Chacko N, Ravichandran M, Rao RR, Shenoi SSC (2012) An anomalous cooling event observed in the Bay of Bengal during June 2009. Ocean Dyn 62(5):671–681. https://doi.org/10.1007/s10236-012-0525-9
Chaigneau A, Le Texier M, Eldin G, Grados C, Pizarro O (2011) Vertical structure of mesoscale eddies in the eastern South Pacific Ocean: a composite analysis from altimetry and argo profiling floats. J Geophys Research: Oceans 116(C11). https://doi.org/10.1029/2011JC007134
Chaitanya AVS, Durand F, Mathew S, Gopalakrishna VV, Papa F, Lengaigne M, Venkatesan R (2015) Observed year-to-year sea surface salinity variability in the Bay of Bengal during the 2009–2014 period. Ocean Dyn 65(2):173–186. https://doi.org/10.1007/s10236-014-0802-x
Chelton DB, Schlax MG, Samelson RM (2011) Global observations of nonlinear mesoscale eddies. Prog Oceanogr 91(2):167–216. https://doi.org/10.1016/j.pocean.2011.01.002
Cheng X, Xie SP, McCreary JP, Qi Y, Du Y (2013) Intraseasonal variability of sea surface height in the Bay of Bengal. J Geophys Research: Oceans 118(2):816–830. https://doi.org/10.1002/jgrc.20075
Colas F, McWilliams JC, Capet X, Kurian J (2012) Heat balance and eddies in the Peru-Chile current system. Clim Dyn 39(1):509–529. https://doi.org/10.1007/s00382-011-1170-6
Dandapat S, Gnanaseelan C, Parekh A (2020) Impact of excess and deficit river runoff on Bay of Bengal upper ocean characteristics using an ocean general circulation model. Deep Sea Res Part II 172:104714. https://doi.org/10.1016/j.dsr2.2019.104714
de Boyer Montégut C, Madec G, Fischer AS, Lazar A, Iudicone D (2004) Mixed layer depth over the global ocean: an examination of profile data and a profile-based climatology. J Geophys Research: Oceans 109(C12). https://doi.org/10.1029/2004JC002378
de Boyer Montégut C, Mignot J, Lazar A, Cravatte S (2007) Control of salinity on the mixed layer depth in the world ocean: 1. General description. J Geophys Research: Oceans 112(C6). https://doi.org/10.1029/2006JC003953
Faghmous JH, Frenger I, Yao Y, Warmka R, Lindell A, Kumar V (2015) A daily global mesoscale ocean eddy dataset from satellite altimetry. Sci data 2(1):1–16. https://doi.org/10.1038/sdata.2015.28
Frenger I, Gruber N, Knutti R, Münnich M (2013) Imprint of Southern Ocean eddies on winds, clouds and rainfall. Nat Geosci 6(8):608–612. https://doi.org/10.1038/ngeo1863
Gaube P, McGillicuddy J Jr, D., Moulin AJ (2019) Mesoscale eddies modulate mixed layer depth globally. Geophys Res Lett 46(3):1505–1512. https://doi.org/10.1029/2018GL080006
George JV, Vinayachandran PN, Vijith V, Thushara V, Nayak AA, Pargaonkar SM, Matthews AJ (2019) Mechanisms of barrier layer formation and erosion from in situ observations in the Bay of Bengal. J Phys Oceanogr 49(5):1183–1200. https://doi.org/10.1175/JPO-D-18-0204.1
Girishkumar MS, Ravichandran M, McPhaden MJ (2013) Temperature inversions and their influence on the mixed layer heat budget during the winters of 2006–2007 and 2007–2008 in the Bay of Bengal. J Geophys Research: Oceans 118(5):2426–2437. https://doi.org/10.1002/jgrc.20192
Girishkumar MS, Joseph J, Thangaprakash VP, Pottapinjara V, McPhaden MJ (2017) Mixed layer temperature budget for the northward propagating summer monsoon intraseasonal oscillation (MISO) in the central Bay of Bengal. J Geophys Research: Oceans 122(11):8841–8854. https://doi.org/10.1002/2017JC013073
Gordon AL, Shroyer E, Murty VSN (2017) An Intrathermocline Eddy and a tropical cyclone in the Bay of Bengal. Sci Rep 7(1):1–8. https://doi.org/10.1038/srep46218
Guinehut S, Dhomps AL, Larnicol G, Le Traon PY (2012) High resolution 3-D temperature and salinity fields derived from in situ and satellite observations. Ocean Sci 8(5):845–857. https://doi.org/10.5194/os-8-845-2012
Gulakaram VS, Vissa NK, Bhaskaran PK (2018) Role of mesoscale eddies on atmospheric convection during summer monsoon season over the Bay of Bengal: a case study. J Ocean Eng Sci 3(4):343–354. https://doi.org/10.1016/j.joes.2018.11.002
Gulakaram VS, Vissa NK, Bhaskaran PK (2020) Characteristics and vertical structure of oceanic mesoscale eddies in the Bay of Bengal. Dyn Atmos Oceans 89:101131. https://doi.org/10.1016/j.dynatmoce.2020.101131
Gulakaram VS, Vissa NK, Bhaskaran PK (2023) Mesoscale eddies with anomalous sea surface temperature and its relation with atmospheric convection over the North Indian Ocean. Int J Climatol 1–20. https://doi.org/10.1002/joc.8018
Hausmann U, McGillicuddy Jr DJ, Marshall J (2017) Observed mesoscale eddy signatures in Southern Ocean surface mixed-layer depth. J Geophys Research: Oceans 122(1):617–635. https://doi.org/10.1002/2016JC012225
He Q, Zhan H, Cai S (2020) Anticyclonic eddies enhance the winter barrier layer and surface cooling in the Bay of Bengal. J Geophys Research: Oceans 125(10):e2020JC016524. https://doi.org/10.1029/2020JC016524
Huang RX (2015) Heaving modes in the world oceans. Clim Dyn 45:3563–3591. https://doi.org/10.1007/s00382-015-2557-6
Jacob SD, Shay LK (2003) The role of oceanic mesoscale features on the tropical cyclone–induced mixed layer response: a case study. J Phys Oceanogr 33(4):649–676. https://doi.org/10.1175/1520-0485(2003)33<649:TROOMF>2.0.CO;2
Kara AB, Rochford PA, Hurlburt HE (2000) An optimal definition for ocean mixed layer depth. J Geophys Research: Oceans 105(C7):16803–16821. https://doi.org/10.1029/2000JC900072
Kara AB, Rochford PA, Hurlburt HE (2003) Mixed layer depth variability over the global ocean. J Geophys Research: Oceans 108(C3). https://doi.org/10.1029/2000JC000736
Keerthi MG, Lengaigne M, Vialard J, de Boyer Montégut C, Muraleedharan PM (2013) Interannual variability of the Tropical Indian Ocean mixed layer depth. Clim Dyn 40(3):743–759. https://doi.org/10.1007/s00382-012-1295-2
Keerthi MG, Lengaigne M, Drushka K, Vialard J, de Boyer Montégut C, Pous S, Muraleedharan PM (2016) Intraseasonal variability of mixed layer depth in the tropical Indian Ocean. Clim Dyn 46(7):2633–2655. https://doi.org/10.1007/s00382-015-2721-z
Kouketsu S, Kaneko H, Okunishi T, Sasaoka K, Itoh S, Inoue R, Ueno H (2016) Mesoscale eddy effects on temporal variability of surface chlorophyll a in the Kuroshio Extension. J Oceanogr 72:439–451. https://doi.org/10.1007/s10872-015-0286-4
Krishnamohan KS, Vialard J, Lengaigne M, Masson S, Samson G, Pous S, Madec G (2019) Is there an effect of Bay of Bengal salinity on the northern Indian Ocean climatological rainfall? Deep Sea Res Part II 166:19–33. https://doi.org/10.1016/j.dsr2.2019.04.003
Kumari A, Kumar SP, Chakraborty A (2018) Seasonal and interannual variability in the barrier layer of the Bay of Bengal. J Geophys Research: Oceans 123(2):1001–1015. https://doi.org/10.1002/2017JC013213
Le Traon P-Y, Ali A, Alvarez Fanjul E, Aouf L, Axell L, Aznar R, Ballarotta M, Behrens A, Mounir B, Bentamy A, Bertino L, Bowyer P, Brando V, Breivik L, Nardelli B, Cailleau B, Ciliberti S, Clementi S, Colella E, Zuo S (2017) H., The Copernicus Marine Environmental Monitoring Service: Main Scientific Achievements and Future Prospects. Mercat. Ocean J. 56.
Locarnini MM, Mishonov AV, Baranova OK, Boyer TP, Zweng MM, Garcia HE, Smolyar I (2018) World ocean atlas 2018, vol 1. Temperature
Mahadevan A (2016) The impact of submesoscale physics on primary productivity of plankton. Annual Rev Mar Sci 8:161–184. https://doi.org/10.1146/annurev-marine-010814-015912
Mahadevan A, Jaeger GS, Freilich M, Omand MM, Shroyer EL, Sengupta D (2016) Freshwater in the Bay of Bengal: its fate and role in air-sea heat exchange. Oceanography 29(2):72–81. http://www.jstor.org/stable/24862671
Mathew S, Natesan U, Latha G, Venkatesan R, Rao RR, Ravichandran M (2018) Observed warming of sea surface temperature in response to tropical cyclone Thane in the Bay of Bengal. Curr Sci, 1407–1413. http://www.jstor.org/stable/26495495
McWilliams JC (2016) Submesoscale currents in the ocean. Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 472(2189), 20160117. https://doi.org/10.1098/rspa.2016.0117
Mulet S, Rio MH, Mignot A, Guinehut S, Morrow R (2012) A new estimate of the global 3D geostrophic ocean circulation based on satellite data and in-situ measurements. Deep Sea Res Part II 77:70–81. https://doi.org/10.1016/j.dsr2.2012.04.012
Narvekar J, Kumar SP (2006) Seasonal variability of the mixed layer in the central Bay of Bengal and associated changes in nutrients and chlorophyll. Deep Sea Res Part I 53(5):820–835. https://doi.org/10.1016/j.dsr.2006.01.012
Narvekar J, Prasanna Kumar S (2014) Mixed layer variability and chlorophyll a biomass in the Bay of Bengal. Biogeosciences 11(14):3819–3843. https://doi.org/10.5194/bg-11-3819-2014
Pant V, Girishkumar MS, Bhaskar U, Ravichandran TVS, Papa M, F., Thangaprakash VP (2015) Observed interannual variability of near-surface salinity in the B ay of B Engal. J Geophys Research: Oceans 120(5):3315–3329. https://doi.org/10.1002/2014JC010340
Parampil SR, Gera A, Ravichandran M, Sengupta D (2010) Intraseasonal response of mixed layer temperature and salinity in the Bay of Bengal to heat and freshwater flux. J Geophys Research: Oceans 115(C5). https://doi.org/10.1029/2009JC005790
Pirro A, Wijesekera HW, Jarosz E, Fernando HJS (2020) Dynamics of intraseasonal oscillations in the Bay of Bengal during summer monsoons captured by mooring observations. Deep Sea Res Part II 172:104718. https://doi.org/10.1016/j.dsr2.2019.104718
Prasad TG (2004) A comparison of mixed-layer dynamics between the Arabian Sea and Bay of Bengal: one‐dimensional model results. J Geophys Research: Oceans 109(C3). https://doi.org/10.1029/2003JC002000
Praveen Kumar B, Vialard J, Lengaigne M, Murty VSN, Mcphaden MJ (2012) TropFlux: air-sea fluxes for the global tropical oceans—description and evaluation. Clim Dyn 38(7):1521–1543. https://doi.org/10.1007/s00382-011-1115-0
Praveen Kumar B, Vialard J, Lengaigne M, Murty VSN, Mcphaden MJ, Cronin MF, Gopala Reddy K (2013) TropFlux wind stresses over the tropical oceans: evaluation and comparison with other products. Clim Dyn 40(7):2049–2071. https://doi.org/10.1007/s00382-012-1455-4
Ramachandran S, Tandon A (2020). Generation of submesoscale temperature inversions below salinity fronts in the Bay of Bengal. J Geophys Res Oceans 125(12):e2020JC016278. https://doi.org/10.1029/2020jc016278
Rao RR, Sivakumar R (2003) Seasonal variability of sea surface salinity and salt budget of the mixed layer of the north Indian Ocean. J Geophys Research: Oceans 108(C1):9–1. https://doi.org/10.1029/2001JC000907
Rao SA, Gopalakrishna VV, Shetye SR, Yamagata T (2002) Why were cool SST anomalies absent in the Bay of Bengal during the 1997 Indian Ocean Dipole Event? Geophys Res Lett 29(11):50–51. https://doi.org/10.1029/2001GL014645
Rio M-H, Mulet S, Picot N (2014) Beyond GOCE for the ocean circulation estimate: synergetic use of altimetry, gravimetry, and in situ data provides new insight into geostrophic and Ekman currents. Geophys Res Lett 41:8918–8925. https://doi.org/10.1002/2014GL061773
Roemmich D, Gilson J (2009) The 2004–2008 mean and annual cycle of temperature, salinity, and steric height in the global ocean from the Argo Program. Prog Oceanogr 82(2):81–100. https://doi.org/10.1016/j.pocean.2009.03.004
Schmitt RW, Olson DB (1985) Wintertime convection in warm-core rings: thermocline ventilation and the formation of mesoscale lenses. J Geophys Research: Oceans 90(C5):8823–8837. https://doi.org/10.1029/JC090iC05p08823
Scott RB, Wang F (2005) Direct evidence of an oceanic inverse kinetic energy cascade from satellite altimetry. J Phys Oceanogr 35(9):1650–1666. https://doi.org/10.1175/JPO2771.1
Sengupta D, Bharath Raj GN, Ravichandran M, Lekha S, J., Papa F (2016) Near-surface salinity and stratification in the north Bay of Bengal from moored observations. Geophys Res Lett 43(9):4448–4456. https://doi.org/10.1002/2016GL068339
Shaji C, Iizuka S, Matsuura T (2003) Seasonal variability of near-surface heat budget of selected oceanic areas in the north tropical Indian Ocean. J Oceanogr 59(1):87–103. https://doi.org/10.1023/A:1022872524758
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 Research: Oceans 107(C6):5–1. https://doi.org/10.1029/2000JC000679
Shetye SR, Gouveia AD, Shankar D, Shenoi SSC, Vinayachandran PN, Sundar D, Nampoothiri G (1996) Hydrography and circulation in the western Bay of Bengal during the northeast monsoon. J Geophys Research: Oceans 101(C6):14011–14025. https://doi.org/10.1029/95JC03307
Singh VK, Roxy MK (2022) A review of ocean-atmosphere interactions during tropical cyclones in the north Indian Ocean. Earth Sci Rev 226:103967. https://doi.org/10.1016/j.earscirev.2022.103967
Sree Lekha J, Buckley JM, Tandon A, Sengupta D (2018) Subseasonal dispersal of freshwater in the northern Bay of Bengal in the 2013 summer monsoon season. J Geophys Research: Oceans 123(9):6330–6348. https://doi.org/10.1029/2018JC014181
Su Z, Wang J, Klein P, Thompson AF, Menemenlis D (2018) Ocean submesoscales as a key component of the global heat budget. Nat Commun 9(1):775. https://doi.org/10.1038/s41467-018-02983-w
Thadathil P, Muraleedharan PM, Rao RR, Somayajulu YK, Reddy GV, Revichandran C (2007) Observed seasonal variability of barrier layer in the Bay of Bengal. J Geophys Research: Oceans 112(C2). https://doi.org/10.1029/2006JC003651
Thadathil P, Suresh I, Gautham S, Prasanna Kumar S, Lengaigne M, Rao RR, Hegde A (2016) Surface layer temperature inversion in the Bay of Bengal: main characteristics and related mechanisms. J Geophys Research: Oceans 121(8):5682–5696. https://doi.org/10.1002/2016JC011674
Thangaprakash VP, Girishkumar MS, Suprit K, Kumar NS, Chaudhuri D, Dinesh K, Weller RA (2016) What controls seasonal evolution of sea surface temperature in the Bay of Bengal? Mixed layer heat budget analysis using moored buoy observations along 90 E. Oceanography 29(2):202–213. https://www.jstor.org/stable/24862683
Trott CB, Subrahmanyam B, Roman-Stork HL, Murty VSN, Gnanaseelan C (2019) Variability of intraseasonal oscillations and synoptic signals in sea surface salinity in the Bay of Bengal. J Clim 32(20):6703–6728. https://doi.org/10.1175/JCLI-D-19-0178.1
Vialard J, Foltz GR, Mcphaden MJ, Duvel JP, de Boyer Montégut C (2008) Strong Indian Ocean sea surface temperature signals associated with the Madden-Julian Oscillation in late 2007 and early 2008. Geophys Res Lett 35(19). https://doi.org/10.1029/2008GL035238
Vidya PJ, Das S (2017) Contrasting Chl-a responses to the tropical cyclones Thane and Phailin in the Bay of Bengal. J Mar Syst 165:103–114. https://www.sciencedirect.com/science/article/abs/pii/S0924796316300641
Vinayachandran PN, Nanjundiah RS (2009) Indian Ocean sea surface salinity variations in a coupled model. Clim Dyn 33(2):245–263. https://doi.org/10.1007/s00382-008-0511-6
Vinayachandran PN, Murty VSN, Babu R, V (2002) Observations of barrier layer formation in the Bay of Bengal during summer monsoon. J Geophys Research: Oceans 107(C12):SRF–19. https://doi.org/10.1029/2001JC000831
Vissa NK, Satyanarayana ANV, Kumar BP (2012) Response of Upper Ocean during passage of MALA cyclone utilizing ARGO data. Int J Appl Earth Obs Geoinf 14(1):149–159. https://doi.org/10.1016/j.jag.2011.08.015
Vissa NK, Satyanarayana ANV, Prasad Kumar B (2013a) Comparison of mixed layer depth and barrier layer thickness for the Indian Ocean using two different climatologies. Int J Climatol 33(13):2855–2870. https://doi.org/10.1002/joc.3635
Vissa NK, Satyanarayana ANV, Kumar BP (2013b) Response of upper ocean and impact of barrier layer on Sidr cyclone induced sea surface cooling. Ocean Sci J 48(3):279–288. https://doi.org/10.1007/s12601-013-0026-x
Wang X, Han G, Qi Y, Li W (2011) Impact of barrier layer on typhoon-induced sea surface cooling. Dyn Atmos Oceans 52(3):367–385. https://doi.org/10.1016/j.dynatmoce.2011.05.002
Williams RG (1988) Modification of ocean eddies by air-sea interaction. J Geophys Research: Oceans 93(C12):15523–15533. https://doi.org/10.1029/JC093iC12p15523
Wilson EA, Riser SC (2016) An assessment of the seasonal salinity budget for the upper Bay of Bengal. J Phys Oceanogr 46(5):1361–1376. https://doi.org/10.1175/JPO-D-15-0147.1
Yang H, Chen Z, Sun S, Li M, Cai W, Wu L, Gan B (2024) Observations reveal intense air-sea exchanges over Submesoscale Ocean Front. Geophys Res Lett 51(2). https://doi.org/10.1029/2023GL106840. e2023GL106840
Yu L (2011) A global relationship between the ocean water cycle and near-surface salinity. J Geophys Research: Oceans 116(C10). https://doi.org/10.1029/2010JC006937
Yu L, Jin X, Weller RA (2008) Multidecade global flux datasets from the Objectively Analyzed Air-Sea Fluxes (OAFlux) Project: Latent and sensible heat fluxes, ocean evaporation, and related surface meteorological variables. Woods Hole Oceanographic Institution OAFlux Project Tec. In Rep
Zweng MM, Seidov D, Boyer TP, Locarnini M, Garcia HE, Mishonov AV, Smolyar I (2019) World ocean atlas 2018, vol 2. Salinity
Acknowledgements
Authors would like to acknowledge the Ministry of Earth Sciences, Government of India, for providing a research grant (MoES/36/OOIS/Extra/46/2016). The authors would also like to acknowledge Copernicus Marine Environment Monitoring Service for making available sea surface height anomalies data, and daily ocean current velocities. The authors acknowledge the Barcelona Expert Center for SMOS data. Argo data was obtained from Coriolis Operational Oceanography. Authors also acknowledge ESSO-INCOIS-Indian National Centre for Ocean Information Services for providing wind-stress, air-sea fluxes data, and WHOI (Woods Hole Oceanographic Institution) OA flux project for providing evaporation data. World Ocean Atlas 2018 data was also obtained from NCEI-NOAA. The authors would like to acknowledge the Physical Science Division of Earth System Laboratory (ESRL), NOAA, for providing daily Sea surface temperature data.
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Gulakaram, V.S., Vissa, N.K. & Bhaskaran, P.K. Processes responsible for mixed layer variations near mesoscale eddies in the Bay of Bengal. Ocean Dynamics 74, 439–457 (2024). https://doi.org/10.1007/s10236-024-01612-z
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DOI: https://doi.org/10.1007/s10236-024-01612-z