Abstract
Climatologically, the frequency of tropical cyclones (TCs) in the Bay of Bengal (BoB) is higher relative to that over the Arabian Sea (ARB). However, recent years exhibit a greater number of TCs forming in the ARB than in the BoB. During the study period (1982–2019), a significant increasing trend in the intensity, frequency, and duration of cyclonic storms (CS) and very severe CS (VSCS) is observed over the ARB. There is a 52% increase in the frequency of CS during the recent epoch (2001–2019) in the ARB, while there is a decrease of 8% in the BoB. Over the ARB, increment in CS duration is 80% and VSCS is almost threefold in the recent epoch as compared to the past epoch (1982–2000). Also, lifetime maximum intensity and accumulated cyclone energy have increased over the ARB implying an increase in the strength of TCs. The increase in TC duration over the ARB is prominent during May, June, and October and a decrease over the BoB is noted during November. The increase in the duration of TCs in the ARB is associated with an increase in mid-level relative humidity and column averaged (950-150 hPa) moist static energy, which is significantly correlated to an increase in sea surface temperatures and tropical cyclone heat potential in the basin. In the recent epoch, TC genesis is observed at lower latitudes (< 8° N), which is another factor contributing to longer durations of TCs. This increases the probability of TC intensification with the support from other favourable environmental parameters. Significant changes in TC tracks are also noted in May, June, and October due to changes in steering currents.
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References
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. https://doi.org/10.1002/joc.927
Baburaj PP, Abhilash S, Mohankumar K, Sahai AK (2020) On the epochal variability in the frequency of cyclones during the pre-onset and onset phases of the monsoon over the north Indian Ocean. Adv Atmos Sci 37:634–651. https://doi.org/10.1007/s00376-020-9070-5
Balaguru K, Taraphdar S, Leung LR, Foltz GR (2014) Increase in the intensity of postmonsoon Bay of Bengal tropical cyclones. Geophys Res Lett. https://doi.org/10.1002/2014GL060197
Balaji M, Chakraborty A, Mandal M (2018) Changes in tropical cyclone activity in north Indian Ocean during satellite era (1981–2014). Int J Climatol 38:2819–2837. https://doi.org/10.1002/joc.5463
Bell SS, Chand SS, Tory KJ et al (2020) North Indian Ocean tropical cyclone activity in CMIP5 experiments: future projections using a model-independent detection and tracking scheme. Int J Climatol. https://doi.org/10.1002/joc.6594
Bhat GS (2003) Measurement of air–sea fluxes over the Indian Ocean and the Bay of Bengal. J Clim 1:12. https://doi.org/10.1175/1520-0442(2003)016%3c0767:MOASFO%3e2.0.CO;2
Bhatia K, Vecchi G, Murakami H et al (2018) Projected response of tropical cyclone intensity and intensification in a global climate model. J Clim. https://doi.org/10.1175/JCLI-D-17-0898.1
Bhatla R, Raj R, Mall RK (2020) Tropical cyclones over the north Indian Ocean in changing climate. In: Srivastava PK, Singh SK, Mohanty UC, Tad M (eds) Techniques for disaster risk management and mitigation. Wiley, New York, pp 63–76
Bister M, Emanuel KA (2002) Low frequency variability of tropical cyclone potential intensity 1. Interannual to interdecadal variability. J Geophys Res Atmos. https://doi.org/10.1029/2001JD000776
Camargo SJ, Sobel AH (2005) Western North Pacific tropical cyclone intensity and ENSO. J Clim 18:2996–3006. https://doi.org/10.1175/JCLI3457.1
Chu JH, Sampson CR, Levine AS, Fukada E (2002) The JointTyphoon Warning Center tropical cyclone best-tracks 1945–2000. Washington, DC
Daloz AS, Camargo SJ (2018) Is the poleward migration of tropical cyclone maximum intensity associated with a poleward migration of tropical cyclone genesis? Clim Dyn 50:705–715. https://doi.org/10.1007/s00382-017-3636-7
Deo AA, Ganer DW (2015) Tropical cyclone activity over the Indian Ocean in the warmer climate. Int J Sci Res 4:880–886. https://doi.org/10.1007/978-94-007-7720-0
Deo AA, Ganer DW, Nair G (2011) Tropical cyclone activity in global warming scenario. Nat Hazards 59:771–786. https://doi.org/10.1007/s11069-011-9794-8
Dube SK, Rao AD, Sinha PC et al (1997) Storm surge forecasting in the Bay of Bengal and Arabian Sea. Mausam 48:283–304
Elsner JB, Kossin JP, Jagger TH (2008) The increasing intensity of the strongest tropical cyclones. Nature 455:92–95. https://doi.org/10.1038/nature07234
Emanuel K (2005) Increasing destructiveness of tropical cyclones over the past 30 years. Nature 436:686–688. https://doi.org/10.1038/nature03906
Emanuel KA, Neelin JD, Christopher S (1994) On large-scale circulations in convecting atmospheres. Q J R Meteorol Soc 120:1111–1143. https://doi.org/10.1002/qj.49712051902
Evan AT, Camargo SJ (2011) A climatology of Arabian Sea cyclonic storms. J Clim 24:140–158. https://doi.org/10.1175/2010JCLI3611.1
Evan AT, Kossin JP, Chung CE, Ramanathan V (2011) Arabian Sea tropical cyclones intensified by emissions of black carbon and other aerosols. Nature. https://doi.org/10.1038/nature10552
Galarneau TJ, Davis CA (2013) Diagnosing forecast errors in tropical cyclone motion. Mon Weather Rev. https://doi.org/10.1175/MWR-D-12-00071.1
Goldenberg SB, Landsea CW, Mestas-Nuñez AM, Gray WM (2001) The recent increase in Atlantic hurricane activity: causes and implications. Science 293:474–479. https://doi.org/10.1126/science.1060040
Grodsky SA, Bentamy A, Carton JA, Pinker RT (2009) Intraseasonal latent heat flux based on satellite observations. J Clim 22:4539–4556. https://doi.org/10.1175/2009JCLI2901.1
Hersbach H, Bell B, Berrisford P et al (2020) The ERA5 global reanalysis. Q J R Meteorol Soc. https://doi.org/10.1002/qj.3803
Joseph S, Ravichandran M, Kumar BP, Jampana RV, Weiqing H (2017) Ocean atmosphere thermal decoupling in the Eastern Equatorial Indian Ocean. Clim Dyn 49:575–594. https://doi.org/10.1007/s00382-016-3359-1
Kim S-H, Moon I-J, Chu P-S (2020) An increase in global trends of tropical cyclone translation speed since 1982 and its physical causes. Environ Res Lett. https://doi.org/10.1088/1748-9326/ab9e1f
Klotzbach PJ (2006) Trends in global tropical cyclone activity over the past twenty years (1986–2005). Geophys Res Lett 33:1984–1987. https://doi.org/10.1029/2006GL025881
Knaff JA, Sampson CR, DeMaria M (2005) An operational statistical typhoon intensity prediction scheme for the western North Pacific. Weather Forecast 20:688–699. https://doi.org/10.1175/WAF863.1
Knutson T, Camargo SJ, Chan JCL et al (2020) Tropical cyclones and climate change assessment: part 2: projected response to anthropogenic warming. Bull Am Meteorol Soc 101:E303–E322. https://doi.org/10.1175/BAMS-D-18-0189.1
Kotal SD, Kundu PK, Roy Bhowmik SK (2009) Analysis of cyclogenesis parameter for developing and nondeveloping low-pressure systems over the Indian Sea. Nat Hazards 50:389–402. https://doi.org/10.1007/s11069-009-9348-5
Leipper DF, Volgenau LD (1972) Hurricane heat potential of the Gulf of Mexico. J Phys Oceanogr 2(3):218–224
Lin II, Wu CC, Pun IF, Ko DS (2008) Upper-ocean thermal structure and the Western North Pacific category 5 typhoons. Part I: Ocean features and the category 5 typhoons’ intensification. Mon Weather Rev 136:3288–3306. https://doi.org/10.1175/2008MWR2277.1
Marquet P (2015) On the computation of moist-air specific thermal enthalpy. Q J R Meteorol Soc 141:67–84. https://doi.org/10.1002/qj.2335
Mittal R, Tewari M, Radhakrishnan C et al (2019) Response of tropical cyclone Phailin (2013) in the Bay of Bengal to climate perturbations. Clim Dyn 53:2013–2030. https://doi.org/10.1007/s00382-019-04761-w
Mohapatra M, Adhikary S (2011) Modulation of cyclonic disturbances over the North Indian ocean by madden—Julian oscillation. Mausam 62:375–390
Mohapatra M, Vijay Kumar V (2017) Interannual variation of tropical cyclone energy metrics over North Indian Ocean. Clim Dyn 48:1431–1445. https://doi.org/10.1007/s00382-016-3150-3
Mohapatra M, Bandyopadhyay BK, Tyagi A (2014) Construction and quality of best tracks parameters for study of climate change impact on tropical cyclones over the north Indian Ocean during satellite era. In: Mohanty UC, Mohapatra M, Singh OP et al (eds) Monitoring and prediction of tropical cyclones in the Indian Ocean and Climate Change. Springer, Dordrecht, pp 3–17
Murakami H, Sugi M, Kitoh A (2013) Future changes in tropical cyclone activity in the north Indian Ocean projected by the new high-resolution MRI-AGCM. Clim Dyn 40:1949–1968. https://doi.org/10.1007/978-94-007-7720-0_6
Murakami H, Vecchi GA, Underwood S (2017) Increasing frequency of extremely severe cyclonic storms over the Arabian Sea. Nat Clim Chang 7:885–889. https://doi.org/10.1038/s41558-017-0008-6
Murakami H, Delworth TL, Cooke WF et al (2020) Detected climatic change in global distribution of tropical cyclones. Proc Natl Acad Sci USA 117:10706–10714. https://doi.org/10.1073/pnas.1922500117
Neelin JD, Held ID (1987) Modeling tropical convergence based on the moist static energy budget. Mon Weather Rev 115:3–12. https://doi.org/10.1175/1520-0493(1987)115%3c0003:MTCBOT%3e2.0.CO;2
Ng EKW, Chan JCL (2012) Interannual variations of tropical cyclone activity over the north Indian Ocean. Int J Climatol 32:819–830. https://doi.org/10.1002/joc.2304
Ohring G, Gruber A (1983) Satellite radiation observations and climate theory. Adv Geophys 25:237–304. https://doi.org/10.1016/S0065-2687(08)60175-2
Pokhrel S, Dutta U, Rahaman H, Chaudhari H, Hazra A, Saha SK, Veeranjaneyulu C (2020) Evaluation of different heat flux products over the tropical Indian Ocean. Earth Space Sci 7:e2019EA000988. https://doi.org/10.1029/2019EA000988
Rajeevan M, Srinivasan J, Niranjan Kumar K et al (2013) On the epochal variation of intensity of tropical cyclones in the Arabian Sea. Atmos Sci Lett. https://doi.org/10.1002/asl2.447
Rappin ED, Nolan DS, Emanuel KA (2010) Thermodynamic control of tropical cyclogenesis in environments of radiative-convective equilibrium with shear. Q J R Meteorol Soc 136:1954–1971. https://doi.org/10.1002/qj.706
Reddy JP, Sriram D, Gunthe SS et al (2021) Impact of climate change on intense Bay of Bengal tropical cyclones of the post-monsoon season: a pseudo global warming approach. Clim Dyn 56:2855–2879. https://doi.org/10.1007/s00382-020-05618-3
Reynolds RW, Smith TM, Liu C et al (2007) Daily high-resolution-blended analyses for sea surface temperature. J Clim 20:5473–5496. https://doi.org/10.1175/2007JCLI1824.1
Roxy MK, Dasgupta P, McPhaden MJ et al (2019) Twofold expansion of the Indo-Pacific warm pool warps the MJO life cycle. Nature 575:647–651. https://doi.org/10.1038/s41586-019-1764-4
Schreck CJ, Molinari J, Mohr KI (2011) Attributing tropical cyclogenesis to equatorial waves in the western north pacific. J Atmos Sci 68:195–209. https://doi.org/10.1175/2010JAS3396.1
Sharma N, Ali MM (2014) Importance of ocean heat content for cyclone studies. Oceanography 2:124. https://doi.org/10.4172/2332-2632.1000124
Shay LK, Goni GJ, Black PG (2000) Effects of a warm oceanic feature on Hurricane Opal. Mon Weather Rev 128:1366–1383. https://doi.org/10.1175/1520-0493(2000)128%3c1366:eoawof%3e2.0.co;2
Singh OP, Ali Khan TM, Rahman MS (2000) Changes in the frequency of tropical cyclones over the north Indian Ocean. Meteorol Atmos Phys 75:11–20. https://doi.org/10.1007/s007030070011
Singh OP, Khan TMA, Rahman MS (2001) Has the frequency of intense tropical cyclones increased in the north Indian Ocean? Curr Sci 80:575–580
Singh K, Panda J, Rath SS (2019a) Variability in landfalling trends of cyclonic disturbances over North Indian Ocean region during current and pre-warming climate. Theor Appl Climatol 137:417–439. https://doi.org/10.1007/s00704-018-2605-3
Singh K, Panda J, Sahoo M, Mohapatra M (2019b) Variability in tropical cyclone climatology over north Indian Ocean during the period 1891 to 2015. Asia Pac J Atmos Sci 55:269–287. https://doi.org/10.1007/s13143-018-0069-0
Srivastav AK, Sinha Ray KC, De US (2000) Trends in the frequency of cyclonic disturbances and their intensification over Indian Seas. Mausam 51:113–118
Suneeta P, Sadhuram Y (2018) Tropical cyclone genesis potential index for Bay of Bengal during peak post-monsoon (October–November) season including atmosphere–ocean parameters. Mar Geod. https://doi.org/10.1080/01490419.2017.1394404
Wang S, Toumi R (2021) Recent migration of tropical cyclones toward coasts. Science 371:514–517. https://doi.org/10.1126/science.abb9038
Wang B, Xu S, Wu L (2012) Intensified Arabian Sea tropical storms. Nature 489:E1–E2. https://doi.org/10.1038/nature11470
Webster PJ, Holland GJ, Curry JA, Chang HR (2005) Atmospheric science: changes in tropical cyclone number, duration, and intensity in a warming environment. Science 309:1844–1846. https://doi.org/10.1126/science.1116448
Zhang K, Randel WJ, Fu R (2017) Relationships between outgoing longwave radiation and diabatic heating in reanalyses. Clim Dyn 49:2911–2929. https://doi.org/10.1007/s00382-016-3501-0
Acknowledgements
IITM is fully funded by the Ministry of Earth Sciences, Government of India. We thank JTWC for the best track dataset, NOAA for the OISST data set, NCEP-GODAS for ocean subsurface monthly temperature data utilized to calculate TCHP. High resolution ERA5 monthly mean reanalysis data is also acknowledged with thanks. All datasets used for this study are freely available online.
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Deshpande, M., Singh, V.K., Ganadhi, M.K. et al. Changing status of tropical cyclones over the north Indian Ocean. Clim Dyn 57, 3545–3567 (2021). https://doi.org/10.1007/s00382-021-05880-z
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DOI: https://doi.org/10.1007/s00382-021-05880-z
Keywords
- Tropical cyclones
- Climate change
- North Indian Ocean
- Bay of Bengal
- Arabian Sea