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Bay of Bengal branch of Indian summer monsoon and its association with spatial distribution of rainfall patterns over India

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Abstract

Indian summer monsoon rainfall is characterized by a considerable variability on the spatial and temporal scale, though the standard deviation of rainfall on the temporal scale is much smaller (ca. 10% of annual long-term mean) compared with that of the spatial scale. It is known that the seasonal rainfall amplitude over India as well as the statistical properties of the subseasonal variability is strongly linked to the Pacific teleconnection on interannual timescales, such as El Niño-Southern Oscillation (ENSO) and La Niña, and the teleconnection is primarily arising from central and eastern Pacific Ocean. But, the west Pacific controls on the southwest monsoonal flow, and in turn, the modulation of rainfall variability in the subseasonal scale by this low-frequency seasonal to interannual background over India is poorly understood. Here, we examine the moisture pathways by which the spatial pattern of rainfall variability in the subseasonal scale is envisaged to be arising due to the interplay between the Bay of Bengal (BoB) summer monsoon circulation and the South China Sea (SCS) moisture dynamics under different background conditions provided by ENSO or the subseasonal movement of the Inter Tropical Convergence Zone (ITCZ). We observe that the south BoB branch of the summer monsoon could occasionally extend up to 120° E in the SCS and reverse back to Indian mainland. We propose a mechanism by which the south BoB branch interacts with the SCS (viz. western Pacific) atmospheric system, thereby facilitating a pathway of the west Pacific moisture intrusion into the Indian subcontinent. The study concludes that the changes in surface temperature/pressure spatial pattern between India and SCS region play an important role in the distribution of the rainfall. In this study, for the first time, the life cycle of south Bay monsoon flow and its interaction with the SCS are discussed, likely to warrant special attention for modelers trying to understand the spatial distribution of rainfall over India.

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References

  • Achuthavarier D, Krishnamurthy V, Kirtman BP, Huang B (2012) Role of the Indian Ocean in the ENSO– Indian summer monsoon teleconnection in the NCEP Climate Forecast System. J Clim 25:2490–2508. https://doi.org/10.1175/JCLI-D-11-00111.1

    Article  Google Scholar 

  • Adler RF, Huffman GJ, Chang A et al (2003) The version-2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979-present). J Hydrometeorol 4:1147–1167

    Article  Google Scholar 

  • Allan R, Ansell T (2006) A new globally complete monthly historical gridded mean sea level pressure dataset (HadSLP2): 1850-2004. J Clim 19:5816–5842

    Article  Google Scholar 

  • Bhat GS, co-authors (2001) BOBMEX - the Bay of Bengal monsoon experiment. Bull Am Meteorol Soc 82:2217–2243

    Article  Google Scholar 

  • Chakraborty S, Sinha N, Chattopadhyay R, Sengupta S, Mohan PM, Datye A (2016) Atmospheric controls on the precipitation isotopes over the Andaman Islands, Bay of Bengal. Sci Rep 6:19555

    Article  Google Scholar 

  • Chattopadhyay R, Phani R, Sabeerali CT, Dhakate AR, Salunke KD, Mahapatra S, Rao AS, Goswami BN (2015) Influence of extra-tropical sea surface temperature on the Indian summer monsoon: an unexplored source of seasonal predictability. Q J R Meteorol Soc 141:2760–2775

    Article  Google Scholar 

  • Chattopadhyay R, Rao SA, Sabeerali CT, George G, Rao DN, Dhakate A, Salunke K (2016) Large-scale teleconnection patterns of Indian summer monsoon as revealed by CFSv2 retrospective seasonal forecast runs. Int J Climatol 36:3297–3313

    Article  Google Scholar 

  • Dansgaard W (1964) Stable isotopes in precipitation. Tellus 16:436–468

    Article  Google Scholar 

  • Das PK (1968) The monsoons. National Book Trust, New Delhi, pp 225–229

    Google Scholar 

  • Dee DP, Uppala SM, Simmons AJ et al (2011) The ERA-interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137:553–597

    Article  Google Scholar 

  • Fadnavis S, Chattopadhyay R (2017) Linkages of subtropical stratospheric intraseasonal intrusions with Indian summer monsoon deficit rainfall. J Clim 30:5083–5095. https://doi.org/10.1175/JCLI-D-16-0463.1

    Article  Google Scholar 

  • Gadgil S (2000) Monsoon-ocean coupling. Curr Sci 78:309–323

    Google Scholar 

  • Gao RZ, Zhou FX, Fang WD (2000) SST intraseasonal oscillation in the SCS and atmospheric forcing system. Chin J Oceanol Liminol 18:289–296

    Article  Google Scholar 

  • Gill EC, Rajagopalan B, Molnar P (2015) Subseasonal variations in spatial signatures of ENSO on the Indian summer monsoon from 1901 to 2009. J Geophys Res Atmos 120:8165–8185. https://doi.org/10.1002/2015JD023184

    Article  Google Scholar 

  • Gimeno L, Stohl A, Trigo RM, Dominguez F, Yoshimura K, Yu L, Drumond A, Durán-Quesada AM, Nieto R (2012) Oceanic and terrestrial sources of continental precipitation. Rev Geophys 50:RG4003

    Article  Google Scholar 

  • Goswami BN (1987) A mechanism for the west northwest movement of the monsoon depressions. Nature 326:376–370

    Article  Google Scholar 

  • Goswami BN (1994) Dynamical predictability of seasonal monsoon rainfall: problems and prospects. Proc Indian Natl Sci Acad 60:101–120

    Google Scholar 

  • Goswami BN (1997) Chaos and predictability of the Indian summer monsoon. Pramana J Phys 48(2):719–736. https://doi.org/10.1007/BF02845671

    Article  Google Scholar 

  • Goswami BN (2012) South Asian monsoon. In W. K. M. Lau, D. Waliser (Eds.), Intraseasonal variability in the atmosphere-ocean climate system (2d ed., pp. 21–72). Chichester: Springer-Praxis

  • Goswami BN, Ajay Mohan RS (2001) Intraseasonal oscillations and interannual variability of the Indian summer monsoon. J Clim 14:1180–1198

    Article  Google Scholar 

  • Goswami BN, Xavier PK (2005) Dynamics of “internal” interannual variability of the Indian summer monsoon in a GCM. J Geophys Res 110:D24104. https://doi.org/10.1029/2005JD006042

    Article  Google Scholar 

  • Goswami BN, Krishnamurthy V, Annamalai H (1999) A broad scale circulation index for the interannual variability of the Indian summer monsoon. Q J R Meteorol Soc 125:611–633

    Article  Google Scholar 

  • Guhathakurta P, Rajeevan M (2007) Trends in the rainfall pattern over India. Int J Climatol 28:1453–1469

    Article  Google Scholar 

  • Hendon HH, Glick J (1997) Intraseasonal air-sea interaction in the tropical Indian and Pacific Oceans. J Clim 10:647–661

    Article  Google Scholar 

  • Joseph S, Sahai AK, Chattopadhyay R, Goswami BN (2011) Can El Niño–Southern Oscillation (ENSO) events modulate intraseasonal oscillations of Indian summer monsoon? J Geophys Res 116:D20123. https://doi.org/10.1029/2010JD015510

    Article  Google Scholar 

  • Ju J, Slingo JM (1995) The Asian summer monsoon and ENSO. Q J R Meteorol Soc 106:447–462

    Google Scholar 

  • Kalnay M, Kanamitsu M et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Kawamura R (1998) A possible mechanism of the Asian summer monsoon-ENSO coupling. J Meteorol Soc Jpn 76:1009–1027

    Article  Google Scholar 

  • Kawamura R, Matsumura T, Iizuka S (2001) Role of equatorially asymmetric sea surface temperature anomalies in the Indian Ocean in the Asian summer monsoon and El Niño-Southern Oscillation coupling. J Geophys Res 106:4681–4693. https://doi.org/10.1029/2000JD900610

    Article  Google Scholar 

  • Koteswaram P, Rao NSB (1963) Formation and structure of Indian summer monsoon depressions. Aust Meteorol Mag 41:62–75

    Google Scholar 

  • Krishna Kumar K, Hoerling M, Rajagopalan B (2005) Advancing dynamical prediction of Indian monsoon rainfall. Geophys Res Lett 32:L08704. https://doi.org/10.1029/2004GL021979

    Article  Google Scholar 

  • Krishna Kumar K, Balaji R, Hoerling M et al (2006) Unraveling the mystery of Indian monsoon failure during El Niño. Science 314:115–118

    Article  Google Scholar 

  • Krishnamurthy V, Shukla J (2000) Intraseasonal and interannual variability of rainfall over India. J Clim 13:4366–4377

    Article  Google Scholar 

  • Krishnan R, Sugi M (2003) Pacific decadal oscillation and variability of the Indian summer monsoon rainfall. Clim Dyn 21:233–242

    Article  Google Scholar 

  • Krishnan R, Ramesh KV, Samala BK, Meyers G, Slingo JM, Fennessy MJ (2006) Indian Ocean–monsoon coupled interactions and impending monsoon droughts. Geophys Res Lett 33:L08711. https://doi.org/10.1029/2006GL025811

    Article  Google Scholar 

  • Kumar B, Rai SP, Saravana Kumar U et al (2010) Isotopic characteristics of Indian precipitation. Water Resour Res 46:W12548

    Article  Google Scholar 

  • Kutzbach G (1987) Concepts of monsoon physics in historical perspective: The Indian monsoon (seventeenth to early twentieth century). Monsoons, J. S. Fein and P. L. Stephens, (Eds)., John Wiley & Sons, 159–210.

  • Meehl GA (1987) The annual cycle and interannual variability in the tropical Pacific and Indian Ocean regions. Mon Weather Rev 115:27–50

    Article  Google Scholar 

  • Morice CP, Kennedy JJ, Rayner NA, Jones PD (2012) Quantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: the HadCRUT4 dataset. J Geophys Res 117:D08101. https://doi.org/10.1029/2011JD017187

    Article  Google Scholar 

  • Mujumdar M, Sooraj KP, Krishnan R, Preethi B, Joshi MK, Varikoden H, Singh BB, Rajeevan M (2017) Anomalous convective activity over sub-tropical east Pacific during 2015 and associated boreal summer monsoon teleconnections. Clim Dyn 48:4081–4091. https://doi.org/10.1007/s00382-016-3321-2.

    Article  Google Scholar 

  • Neena JM, Suhas E, Goswami BN (2011) Leading role of internal dynamics in the 2009 Indian summer monsoon drought. J Geophys Res 116:D13103. https://doi.org/10.1029/2010JD015328

    Article  Google Scholar 

  • Onogi K, others (2007) The JRA-25 reanalysis. J Meteorol Soc Jpn 85(3):369–432

    Article  Google Scholar 

  • Pai DS, Rajeevan M (2009) Summer monsoon onset over Kerala: new definition and prediction. J Earth Syst Sci 118:123–135

    Article  Google Scholar 

  • Pfahl S, Wernli H (2009) Lagrangian simulations of stable isotopes in water vapor: an evaluation of non-equilibrium fractionation in the Craig-Gordon model. J Geophys Res 114:D20108

    Article  Google Scholar 

  • Rajeevan M, Gadgil S, Bhate J (2010) Active and break spells of the Indian summer monsoon. J Earth Sys Sci 119:229–248

    Article  Google Scholar 

  • Rao YP (1976) Southwest monsoon. Meteorological Monogr, Synoptic Meteorol No. 1/1976, Indian Meteorological Department, Delhi, India

  • Rasmusson EM, Carpenter TH (1982) Variations in tropical sea surface temperature and surface wind field associated with the Southern Oscillation/El Niño. Mon Weather Rev 110:354–384

    Article  Google Scholar 

  • Shinoda T, Hendon HH (1998) Mixed layer modeling of intraseasonal variability in the tropical western Pacific and Indian Oceans. J Clim 11:2668–2685

    Article  Google Scholar 

  • Sikka DR, Dixit CM (1972) A study of satellite observed cloudiness over the equatorial Indian Ocean and India during the southwest monsoon season. J Mar Biol Assoc India 14:805–818

    Google Scholar 

  • Sikka DR, Gadgil S (1980) On the maximum cloud zone and the ITCZ over India longitude during the southwest monsoon. Mon Weather Rev 108:1840–1853

    Article  Google Scholar 

  • Sinha N, Chakraborty S, Chattopadhyay R et al (2018) Isotopic studies of rainfall and its reconstruction using speleothems from the Indian subcontinent. Ph.D. dissertation, Department of Atmospheric and Space Sciences, Savitribai Phule Pune University, Pune, Maharashtra, India

  • Sodemann H, Masson-Delmotte V, Schwierz C, Vinther BM, Wernli H (2008) Interannual variability of Greenland winter precipitation sources: 2. Effects of North Atlantic Oscillation variability on stable isotopes in precipitation. J Geophys Res 113:D12111

    Article  Google Scholar 

  • Stein AF, Draxler RR, Rolph GD, Stunder BJB, Cohen MD, Ngan F (2015) NOAA’s HYSPLIT atmospheric transport and dispersion modelling system. Bull Am Meteorol Soc 96(12):2059–2077

    Article  Google Scholar 

  • Trenberth KE, Stepaniak DP, Caron JM (2000) The global monsoon as seen through the divergent atmospheric circulation. J Clim 13:3969–3993

    Article  Google Scholar 

  • Webster PJ, Yang S (1992) Monsoon and ENSO: selectively interactive systems. Q J R Meteorol Soc 118:877–926

    Article  Google Scholar 

  • Wu R, Kirtman BP (2004) Impacts of the Indian Ocean on the Indian summer monsoon–ENSO relationship. J Clim 17:3037–3054

    Article  Google Scholar 

  • Yang S, Lau KM (1998) Influence of sea surface temperature and ground wetness on Asian summer monsoon. J Clim 11:3230–3246

    Article  Google Scholar 

  • Yasunari T (1979) Cloudiness fluctuations associated with the northern hemisphere summer monsoon. J Meteorol Soc Jpn 57:227–242

    Article  Google Scholar 

  • Yasunari T, Seki Y (1992) Role of the Asian monsoon on the interannual variability of the global climate system. J Meteorol Soc Jpn 70:177–189

    Article  Google Scholar 

  • Zhou FX, Ding J, Yu SY (1995) The intraseasonal oscillation of sea surface temperature in the South China Sea (in Chinese). J Ocean Univ Qingdao 25:1–6

    Google Scholar 

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Acknowledgments

The Indian Institute of Tropical Meteorology, Pune (IITM), is fully supported by the Earth System Science Organization of the Ministry of Earth Sciences, Govt. of India. The authors thank the Director of IITM for providing support and encouragement to carry out this research. We also thank Jyoti Jadhav for her comments on an earlier draft of this manuscript. The figures are prepared using PyFerret.

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Authors and Affiliations

  1. Center for Climate Change Research, Indian Institute of Tropical Meteorology, Pune, 411008, India

    Nitesh Sinha, Rajib Chattopadhyay & S. Chakraborty

  2. Department of Atmospheric and Space Science, Savitribai Phule Pune University, Pune, 411007, India

    Nitesh Sinha & S. Chakraborty

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  1. Nitesh Sinha
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Sinha, N., Chattopadhyay, R. & Chakraborty, S. Bay of Bengal branch of Indian summer monsoon and its association with spatial distribution of rainfall patterns over India. Theor Appl Climatol 137, 1895–1907 (2019). https://doi.org/10.1007/s00704-018-2709-9

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