Ocean Dynamics

, Volume 64, Issue 3, pp 325–335 | Cite as

Observed oceanic response to tropical cyclone Jal from a moored buoy in the south-western Bay of Bengal

  • M. S. Girishkumar
  • K. Suprit
  • Jayaram Chiranjivi
  • T. V. S. Udaya Bhaskar
  • M. Ravichandran
  • R. Venkat Shesu
  • E. Pattabhi Rama Rao
Article

Abstract

Upper oceanographic and surface meteorological time-series observations from a moored buoy located at 9.98°N, 88°E in the south-western Bay of Bengal (BoB) were used to quantify variability in upper ocean, forced by a tropical cyclone (TC) Jal during November 2010. Before the passage of TC Jal, salinity and temperature profiles showed a typical BoB post-monsoon structure with relatively warm (30 °C) and low-saline (32.8 psu) waters in the upper 30- to 40-m layer, and relatively cooler and higher salinity (35 psu) waters below. After the passage of cyclone, an abrupt increase of 1 psu (decrease of 1 °C) in salinity (temperature) in the near-surface layers (up to 40-m depth) was observed from buoy measurements, which persisted up to 10–12 days during the relaxation stage of cyclone. Mixed layer heat budget analysis showed that vertical processes are the dominant contributors towards the observed cooling. The net surface heat flux and horizontal advection together contributed approximately 33 % of observed cooling, during TC Jal forced stage. Analysis showed the existence of strong inertial oscillation in the thermocline region and currents with periodicity of ∼2.8 days. During the relaxation stage of the cyclone, upward movement of thermocline in near-inertial frequencies played significant role in mixed layer temperature and salinity variability, by much freer turbulent exchange between the mixed layer and thermocline.

Keywords

Bay of Bengal Tropical cyclone Upper ocean response 

Notes

Acknowledgments

The encouragement and facilities provided by the Director, INCOIS, are gratefully acknowledged. We would also like to acknowledge two anonymous reviewers, whose comments and suggestions greatly improved the manuscript. Ocean observation programme of the National Institute of Technology (NIOT), Chennai, is gratefully acknowledged for the deployment and maintenance of OMNI buoy. A. Mukherjee provided the wavelet code for calculating rotary spectra. Figures in this manuscript are generated using FERRET. This is INCOIS contribution Number 172.

References

  1. Alam MM, Hossain MA, Shafee S (2003) Frequency of Bay of Bengal cyclonic storms and depressions crossing different coastal zones. Int J Climatol 23:1119–1125. doi:10.1002/joc.927 CrossRefGoogle Scholar
  2. Ali MM, Jagadeesh PSV, Jain S (2007) Effects of eddies on Bay of Bengal cyclone intensity. Eos Trans AGU 88:93–95. doi:10.1029/2007EO080001 CrossRefGoogle Scholar
  3. Anderson SP, Weller RA, Lukas RB (1996) Surface buoyancy forcing and the mixed layer of the western Pacific warm pool: observations and 1D model results. J Clim 9:3056–3085CrossRefGoogle Scholar
  4. 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 U S A 109:14343–14347CrossRefGoogle Scholar
  5. Behera SK, Deo AA, Salvekar PS (1998) Investigation of mixed layer response to Bay of Bengal cyclone using a simple ocean model. Meteorog Atmos Phys 65:77–91CrossRefGoogle Scholar
  6. Bender MA, Ginis I (2000) Real-case simulations of hurricane–ocean interaction using a high-resolution coupled model: effects on hurricane intensity. Mon Weather Rev 128:917–946. doi:10.1175/1520-0493(2000)128<0917:RCSOHO>2.0.CO;2 CrossRefGoogle Scholar
  7. Bender MA, Ginis I, Kurihara Y (1993) Numerical simulations of the tropical cyclone-ocean interaction with a high-resolution coupled model. J Geophys Res 98:23245–23263CrossRefGoogle Scholar
  8. Cione JJ, Uhlhorn EW (2003) Sea surface temperature variability in hurricanes: implications with respect to intensity change. Mon Weather Rev 131:1783–1796. doi:10.1175//2562.1 CrossRefGoogle Scholar
  9. D’Asaro EA, Sanford TB, Niiler PP, Terrill EJ (2007) Cold wake of Hurricane Frances. Geophys Res Lett 34, L15609. doi:10.1029/2007GL030160 CrossRefGoogle Scholar
  10. De Boyer MC, Vialard J, Shenoi SSC, Shankar D, Durand F, Ethe C, Madec G (2007) Simulated seasonal and interannual variability of mixed layer heat budget in the northern Indian Ocean. J Clim 20:3249–3268. doi:10.1175/JPO-D-12-090.1 CrossRefGoogle Scholar
  11. Emanuel KA (1999) Thermodynamic control of hurricane intensity. Nature 401:665–669. doi:10.1038/44326 Google Scholar
  12. Emery WJ, Thomson RE (1998) Data analysis methods in physical oceanography. Pergamon, KidlingtonGoogle Scholar
  13. Fairall CW, Bradley EF, Hare JE, Grachev AA, Edson JB (2003) Bulk parameterization of air-sea fluxes: updates and verification for the COARE algorithm. J Clim 16:571–591CrossRefGoogle Scholar
  14. Foltz GR, McPhaden MJ (2009) Impact of barrier layer thickness on SST in the Central Tropical North Atlantic. J Clim 22:285–299. doi:10.1175/2008JCLI2308.1 CrossRefGoogle Scholar
  15. Fu LL (1981) Observations and models of inertial waves in the deep ocean. Rev Geophys Space Phys 19:141–170Google Scholar
  16. Gentemann CL, Wick GA, Cummings J, Bayler E (2004) Multi-sensor improved sea surface temperature (MISST) for GODAE, presented at 13th Conference on Satellite Meteorology and Oceanography, Norfolk, VA, USA, 19–23, September,2004. URL http://www.remss.com/papers/gentemann/gentemann_13satmet_2004.pdf
  17. Gerkema T, Maas LRM, vanHaren H (2013) A note on the role of mean flows in doppler-shifted frequencies. J Phys Oceanogr 43:432–441CrossRefGoogle Scholar
  18. Girishkumar MS, Ravichandran M, Rao RR, McPhaden MJ (2011) Intraseasonal variability in barrier layer thickness in the south central Bay of Bengal. J Geophys Res 116, C03009. doi:10.1029/2010JC006657 Google Scholar
  19. Girishkumar MS, Ravichandran M, McPhaden MJ (2013a) 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 Res Oceans 118:2426–2437. doi:10.1002/jgrc.20192 CrossRefGoogle Scholar
  20. Girishkumar MS, Ravichandran M, Han W (2013b) Observed intraseasonal thermocline variability in the Bay of Bengal. J Geophys Res Oceans 118:3336–3349. doi:10.1002/jgrc.20245 CrossRefGoogle Scholar
  21. Huffman GJ, Adler RF, Bolvin DT, Gu GJ, Nelkin EJ, Bowman KP, Hong Y, Stocker EF, Wolff DB (2007) The TRMM multisatellite precipitation analysis (TMPA): quasi-global, multiyear, combined-sensor precipitation estimates at fine scales. J Hydromet 8:38–55CrossRefGoogle Scholar
  22. Jacob SD, Koblinsky C (2007) Effects of precipitation on the upper-ocean response to a hurricane. Mon Weather Rev 135:2207–2225CrossRefGoogle Scholar
  23. Jourdain NC, Lengaigne M, Vialard J, Madec G, Menkes CE, Vincent EM, Samson G, Jullien Barnier B (2013) Observation-based estimates of ocean mixing inhibition by heavy rainfall under tropical cyclones. J Phys Oceanogr 43:205–221CrossRefGoogle Scholar
  24. Kaplan J, DeMaria MJ, Knaff A (2010) A revised tropicalcyclone rapid intensification index for the Atlantic and eastern North Pacific Basins. Weather Forecast 25:220–241. doi:10.1175/2009WAF2222280.1 CrossRefGoogle Scholar
  25. Lin II, Chen CH, Pun IF, Liu T, Wu CCW (2009) Warm ocean anomaly, air sea fluxes, and the rapid intensification of tropical cyclone Nargis (2008). Geophys Res Lett 36, L03817. doi:10.1029/2008GL035815 Google Scholar
  26. Liu PC, Miller GS (1996) Wavelet transforms and ocean current data analysis. J Atmos Ocean Technol 13:1090–1099. doi:10.1175/1520-0426(1996)013<1090:WTAOCD>2.0.CO;2 CrossRefGoogle Scholar
  27. Lloyd ID, Vecchi GA (2011) Observational evidence for oceanic controls on hurricane intensity. J Clim 24:1138–1153. doi:10.1175/2010JCLI3763.1 CrossRefGoogle Scholar
  28. Lukas R, Lindstrom E (1991) The mixed layer of the western equatorial Pacific Ocean. J Geophys Res 96:3343–3357CrossRefGoogle Scholar
  29. Maneesha K, Murty VSN, Ravichandran M, Lee T, Yu W, McPhaden MJ (2012) Upper ocean variability in the Bay of Bengal during the tropical cyclones Nargis and Laila. Prog Oceanogr 106:49–61CrossRefGoogle Scholar
  30. McCreary JP, Kundu PK, Molinari RL (1993) A numerical investigation of dynamics, thermodynamics and the mixed layer processes in the Indian Ocean. Prog Oceanogr 31:181–244CrossRefGoogle Scholar
  31. McPhaden MJ, Foltz GR, Lee T, Murty VSN, Ravichandran M, Vecchi GA, Vialard J, Wiggert JD, Yu L (2009) Ocean–atmosphere interactions during cyclone Nargis. EOS Trans AGU 90:53–54. doi:10.1029/2009EO070001 CrossRefGoogle Scholar
  32. Mignot J, Lazar A, Lacarra M (2012) On the formation of barrier layers and associated vertical temperature inversions: a focus on the northwestern tropical Atlantic. J Geophys Res 117, C02010. doi:10.1029/2011JC007435 Google Scholar
  33. Morel A, Antoine D (1994) Heating rate within the upper ocean in relation to its bio-optical state. J Phys Oceanogr 24:1652–1665CrossRefGoogle Scholar
  34. Mukherjee A, Shankar D, Aparna SG, Amol P, Fernando V, Fernandes R, Khalap S, Narayan S, Agarvadekar Y, Gaonkar M, Tari P, Kankonkar A, Vernekar S (2013) Near-inertial currents off the east coast of India. Cont Shelf Res 55:29–39CrossRefGoogle Scholar
  35. Neetu S, Lengaigne M, Vincent EM, Vialard J, Madec G, Samson G, Ramesh Kumar MR, Durand F (2012) Influence of oceanic stratification on tropical cyclones-induced surface cooling in the Bay of Bengal. J Geophys Res 117. doi:10.1029/2012JC008433
  36. Prasad TG, Hogan PJ (2007) Upper-ocean response to Hurricane Ivan in a 1/25° nested Gulf of Mexico HYCOM. J Geophys Res 112. doi:10.1029/2006JC003695
  37. Price JF (1981) Upper-ocean response to a hurricane. J Phys Oceanogr 11:153–175CrossRefGoogle Scholar
  38. Price JF (1983) Internal wave wake of a moving storm. Part I: scales, energy budget, and observations. J Phys Oceanogr 13:949–965CrossRefGoogle Scholar
  39. Price JF, Sanford TB, Forristall GZ (1994) Forced stage response to a moving hurricane. J Phys Oceanogr 24:233–260CrossRefGoogle Scholar
  40. Rao AD, Madhu J, Jain I, Ravichandran M (2010) Response of subsurface waters in the eastern Arabian Sea to tropical cyclones. Estuarine Coast Shelf Sci 89:267–276. doi:10.1016/j.ecss.2010.07.011 Google Scholar
  41. 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 Res 108(C1):3009. doi:10.1029/2001JC000907 CrossRefGoogle Scholar
  42. Rao RR, Rao DS, Murthy PGK, Joseph MX (1983) A preliminary investigation of the summer monsoonal forcing on the thermal structure of upper Bay of Bengal during Monex-79. Mausum 32:85–92Google Scholar
  43. Schade LR (2000) Tropical cyclone intensity and sea surface temperature. J Atmos Sci 57:3122–3130CrossRefGoogle Scholar
  44. Sengupta D, Goddalehundi BR, Anitha DS (2007) Cyclone-induced mixing does not cool SST in the post-monsoon north Bay of Bengal. Atmos Sci Lett 9:1–6CrossRefGoogle Scholar
  45. 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):3052. doi:10.1029/2000JC000679 CrossRefGoogle Scholar
  46. Shesu RV, Udaya Bhaskar TVS, Pattabhi Rama Rao E, Devender R, Hemasundar Rao T (2013) Open source architecture for web-based oceanographic data services. Data Sci J 12:47–55CrossRefGoogle Scholar
  47. Shetye SR, Gouveia AD, Shankar D, Shenoi SSC, Vinayachandran P, Sundar D, Michael GS, Namboodiri G (1996) Hydrography and circulation in the western Bay of Bengal during the northeast monsoon. J Geophys Res 101:14011–14025CrossRefGoogle Scholar
  48. Subramanyam B, Murthy VSN, Sharp RJ, O’Brien JJ (2005) Air-Sea coupling during the tropical cyclones in the Indian Ocean: a case study using satellite observations. Pure Appl Geophys 162:1643–1672CrossRefGoogle Scholar
  49. Suryanarayana A, Murty VSN, Rao DP (1993) Hydrography and circulation of the Bay of Bengal during early winter, 1983. Deep Sea Res 40(1):205–217CrossRefGoogle Scholar
  50. Sweeney C, Gnanadesikan A, Griffies S, Harrison M, Rosati A, Samuels B (2005) Impacts of shortwave penetration depth on largescale ocean circulation heat transport. J Phys Oceanogr 35:1103–1119. doi:10.1175/JPO2740.1 Google Scholar
  51. Thadathil P, Gopalakrishna VV, Muraleedharan PM, Reddy GV, Araligidad N, Shenoy S (2002) Surface layer temperature inversion in the Bay of Bengal. Deep-Sea Res 49:1801–1818CrossRefGoogle Scholar
  52. Thadathil P, Muraleedharan PM, Rao RR, Somayajulu YK, Reddy GV, Revichandran C (2007) Observed seasonal variability ofbarrier layer in the Bay of Bengal. J Geophys Res 112, C02009. doi:10.1029/2006JC003651 Google Scholar
  53. Thompson B, Gnanaseelan C, Salvekar PS (2006) Seasonal evolution of temperature inversions in the north Indian Ocean. Curr Sci 90:697–704Google Scholar
  54. Torrence C, Compo GP (1998) A practical guide to wavelet analysis. Bull Am Meteorol Soc 79:61–78CrossRefGoogle Scholar
  55. Venkatesan R, Shamji VR, Latha G, Mathew S, Rao RR, Muthiah A, Atmanand MA (2013) In situ ocean subsurface time-series measurements from OMNI buoy network in the Bay of Bengal. Curr Sci 104:1166–1177Google Scholar
  56. Vialard J, Foltz GR, McPhaden MJ, Duvel JP, Montegut CB (2008) Strong Indian Ocean sea surface temperature signals associated with the Madden-Julian Oscillation in late 2007 and early 2008. Geophys Res Lett 35, L19608. doi:10.1029/2008GL035238 CrossRefGoogle Scholar
  57. Vinayachandran PN, Murty VSN, Ramesh Babu V (2002) Observations of barrier layer formation in the Bay of Bengal during summer monsoon. J Geophys Res 107:8018. doi:10.1029/2001JC000831 CrossRefGoogle Scholar
  58. Vinayachandran PN, Shankar D, Vernekar S, Sandeep KK, Amol P, Neema CP, Chatterjee A (2013) A summer monsoon pump to keep the Bay of Bengal salty. Geophys Res Lett 40:1777–1782. doi:10.1002/grl.50274 CrossRefGoogle Scholar
  59. Vincent EM, Lengaigne M, Madec G, Vialard J, Samson G, Jourdain N, Menkes CE, Jullien S (2012a) Processes setting the characteristics of sea surface cooling induced by Tropical Cyclones. J Geophys Res 117, C02020. doi:10.1029/2011JC007396 Google Scholar
  60. Vincent EM, Lengaigne M, Vialard J, Madec G, Jourdain N, Masson S (2012b) Assessing the oceanic control on the amplitude of sea surface cooling induced by Tropical Cyclones. J Geophys Res 117: doi: 10.1029/2011JC007705
  61. Wang Z, DiMarco SF, Stoessel MM, Zhang X, Howard MK, du Vall K (2012) Oscillation responses to tropical Cyclone Gonu in northern Arabian Sea from a moored observing system. Deep-Sea Res 64:129–145CrossRefGoogle Scholar
  62. Yablonsky RM, Ginis I (2013) Impact of a Warm Ocean Eddy’s Circulation on Hurricane-Induced Sea Surface Cooling with Implications for Hurricane Intensity. Mon Weather Rev 141:9971021. doi:10.1175/MWR-D-12-00248.1 CrossRefGoogle Scholar
  63. Zhu T, Zhang DL (2006) The impact of the storm-induced SST cooling on hurricane intensity. Adv Atmos Sci 23:14–22CrossRefGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  • M. S. Girishkumar
    • 1
    • 3
  • K. Suprit
    • 1
  • Jayaram Chiranjivi
    • 2
  • T. V. S. Udaya Bhaskar
    • 1
  • M. Ravichandran
    • 1
  • R. Venkat Shesu
    • 1
  • E. Pattabhi Rama Rao
    • 1
  1. 1.Indian National Centre for Ocean Information ServicesHyderabadIndia
  2. 2.Regional Remote Sensing Centre - East, NRSC, ISROKolkataIndia
  3. 3.Indian National Centre for Ocean Information Services (INCOIS)HyderabadIndia

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