Abstract
This work attempts to reconcile in a common and comprehensive framework the various conflicting results found in the literature regarding Indian Summer Monsoon (ISM) rainfall-Sea Surface Temperature (SST) relationships, especially the links with El-Niño Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD). To do so, we first examine the linear relationships between ISM rainfall and global SST anomalies during 1950–1976 and 1979–2006 periods. Our results highlight the existence of significant modulations in SST teleconnections and precursory patterns between the first (June–July, JJ) and second part (August–September, AS) of the monsoon. This JJ–AS rainfall dichotomy is more pronounced after the 1976–1977 climate regime shift and tends to blur the global ISM-ENSO signal during the recent period, leading to an apparent weakening of this relationship at the seasonal time scale. Although ISM rainfall in JJ and AS is still strongly linked to ENSO over both periods, the lead-lag relationships between ENSO and AS Indian rainfall have changed during recent decades. Indeed, ENSO variability in the preceding boreal winter has now a significant impact on rainfall variability during the second half of ISM. To evaluate in more details the impact of this JJ-AS dichotomy on the ISM-ENSO-IOD relationships, ISM correlations are also examined separately during El Niño and La Niña years. Results indicate that the early onset of El Niño during boreal spring causes deficient monsoon rainfall in JJ. In response to weaker monsoon winds, warm SST anomalies appear in the west equatorial IO, generating favorable conditions for the development of a positive IOD in AS. Local air-sea processes triggered by the SST anomalies in the eastern node of IOD seem, in turn, to have a more active role on AS rainfall variability, as they may counteract the negative effect of El Niño on ISM rainfall via a modulation of the local Hadley circulation in the eastern IO. The JJ–AS rainfall dichotomy and its recent amplification may then result from an enhancement of these IO feedbacks during recent El Niño years. This explains why, although El Niño events are stronger, a weakening of the ISM-ENSO relationship is observed at the seasonal scale after 1979. Results during La Niña years are consistent with this hypothesis although local processes in the southeast IO now play a more prominent role and act to further modulate ISM rainfall in AS. Finally, our results highlight the existence of a biennal rhythm of the IOD-ENSO-ISM system during the recent period, according to which co-occurring El Niño and positive IOD events tend to be followed by a warming of the IO, a wet ISM during summer and, finally, a La Niña event during the following boreal winter.
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References
Abram NJ, Gagan MK, Cole JE, Hantoro WS, Mudelsee M (2008) Recent intensification of tropical climate variability in the Indian Ocean. Nat Geosci 1:849–853
Alexander MA, Vimont DJ, Chang P, Scott JD (2010) The impact of extra tropical atmospheric variability on ENSO: testing the seasonal foot printing mechanism using coupled model experiments. J Clim 23:2885–2901
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
Alory G, Wijffels S, Meyers G (2007) Observed temperature trends in the Indian Ocean over 1960–1999 and associated mechanisms. Geophys Res Lett 34:L02606. doi:10.1029/2006GL028044
Annamalai H, Liu P (2005) Response of the Asian summer monsoon to changes in El Niño properties. Q J R Meteorol Soc 131:805–831
Annamalai H, Hamilton K, Sperber KR (2007) The South Asian summer monsoon and its relationship with ENSO in the IPCC AR4 simulations. J Clim 20:1071–1092
Ashok K, Guan Z, Yamagata T (2001) Influence of the Indian Ocean dipole on the relationship between the Indian monsoon rainfall and ENSO. Geophys Res Lett 28:4499–4502
Ashok K, Guan Z, Saji NH, Yamagata T (2004) Individual and combined influences of ENSO and the Indian Ocean dipole on the Indian summer monsoon. J Clim 17:3141–3154
Ashrit RG, Douville H, Rupa Kumar K (2003) Response of the Indian monsoon and ENSO-monsoon teleconnection to enhanced greenhouse effect in the CNRM coupled model. J Meteor Soc Jpn 81:779–803
Behera SK, Yamagata T (2001) Subtropical SST dipole events in the southern Indian Ocean. Geophys Res Lett 28:327–330
Blanford HF (1884) On the connexion of Himalaya snowfall and seasons of drought in India. Proc R Soc Lond 37:3–22
Boschat G, Terray P, Masson S (2010) Interannual relationships between Indian summer monsoon and Indo-Pacific coupled modes of variability during recent decades. Clim Dyn. doi:10.1007/s00382-010-0887-y
Cai W, Sullivan A, Cowan T (2009a) Rainfall teleconnections with Indo-Pacific variability in the WCRP CMIP3. Model J Clim 22:5046–5071
Cai W, Cowan T, Sullivan A (2009b) Recent unprecedented skewness towards positive Indian Ocean dipole occurrences and its impact on Australian rainfall. Geophys Res Lett 36:L11705. doi:10.1029/2009GL037604
Cai W, Sullivan A, Cowan T (2009c) Climate change contributes to more frequent consecutive positive Indian Ocean dipole events. Geophys Res Lett 36:L23704. doi:10.1029/2009GL040163
Chang P et al (2006) Climate fluctuations of tropical coupled systems—the role of ocean dynamics. J Clim 19:5122–5174
Clark CO, Cole JE, Webster PJ (2000) Indian Ocean SST and Indian summer rainfall: predictive relationships and their decadal variability. J Clim 13:2503–2519
Cleveland RB, Cleveland WS, McRae JE, Terpenning I (1990) A seasonal-trend decomposition procedure based on loess (with discussion). J Off Stat 6:3–73
Drbohlav HKL, Gualdi S, Navarra A (2007) A diagnostic study of the Indian Ocean dipole mode in El Niño and non-El Niño years. J Clim 20:2961–2977
Du Y, Xie S-P, Huang G, Hu K-M (2009) Role of air–sea interaction in the long persistence of El Niño -induced North Indian Ocean warming. J Clim 22:2023–2038
Ebisuzaki W (1997) A method to estimate the statistical significance of a correlation when the data are serially correlated. J Clim 10:2147–2153
Fedorov AV, Philander SG (2000) Is El Niño changing? Science 288:1997–2002. doi:10.1126/science.288.5473.1997
Fedorov AV, Philander SG (2001) A stability analysis of tropical ocean-atmosphere interactions: bridging measurements and theory for El Niño. J Clim 14:3086–3101
Fischer AS, Terray P, Delecluse P, Gualdi S, Guilyardi E (2005) Two independent triggers for the Indian Ocean dipole/zonal mode in a coupled GCM. J Clim 18:3428–3449
Francis PA, Gadgil S (2010) Towards understanding the unusual Indian monsoon in 2009. J Earth Syst Sci 119:397–415
Gadgil S, Vinayachandran PN, Francis PA, Gadgil S (2004) Extremes of the Indian summer monsoon rainfall, ENSO and equatorial Indian Ocean oscillation. Geophys Res Lett 31:L12213. doi:10.1029/2004GL019733
Gadgil S, Rajeevan M, Nanjundiah R (2005) Monsoon prediction—why yet another failure? Curr Sci 84:1713–1719
Gadgil S, Rajeevan M, Francis PA (2007) Monsoon variability: links to major oscillations over the equatorial Pacific and Indian oceans. Curr Sci 93:182–194
Gershunov A, Schneider N, Barnett T (2000) Low-frequency modulation of the ENSO-Indian monsoon rainfall relationship: signal or noise? J Clim 14:2486–2492
Hong CC, Lu MM, Kanamitsu M (2008) Temporal and spatial characteristics of positive and negative Indian Ocean dipole with and without ENSO. J Geophys Res 113:DO8107. doi:10.1029/2007JD009151
Hong CC, Li T, Lin HO, Chen YC (2010) Asymmetry of the Indian Ocean basin wide SST anomalies: roles of ENSO and IOD. J Clim 23:3563–3576
Hurrell JW, Trenberth KE (1999) Global sea surface temperature analyses: multiple problems and their implications for climate analysis, modeling and reanalysis. Bull Amer Met Soc 80:2661–2678
Ihara C, Kushnir Y, Cane MA, de la Pena V (2007) Indian summer monsoon rainfall and its link with ENSO and the Indian Ocean climate indices. Int J Clim 27:179–187
Ihara C, Kushnir Y, Cane MA (2008) Warming trend of the Indian Ocean SST and Indian Ocean dipole from 1880 to 2004. J Clim 21:2035–2046
Ihara C, Kushnir Y, Cane MA, Victor HP (2009) Climate change over the equatorial Indo-Pacific in global warming. J Clim 22:2678–2693
Izumo T, De Boyer Montégut C, Luo J-J, Behera SK, Masson S, Yamagata T (2008) The role of the Western Arabian Sea upwelling in Indian monsoon rainfall variability. J Clim 21:5603–5623
Ju J, Slingo JM (1995) The Asian summer monsoon and ENSO. Quart J Roy Meteor Soc 121:1133–1168
Kinter JL, Miyakoda K, Yang S (2002) Recent change in the connection from the Asian monsoon to ENSO. J Clim 15:1203–1215
Kinter J, Fennessy M, Krishnamurthy V, Marx L (2004) An evaluation of the apparent interdecadal shift in the tropical divergent circulation in the NCEP-NCAR reanalysis. J Clim 17:349–361
Krishna Kumar K, Rajagopalan B, Cane M (1999) On the weakening relationship between the Indian monsoon and ENSO. Science 284:2156–2159
Krishna Kumar K, Hoerling M, Rajagopalan B (2005) Advancing dynamical prediction of Indian monsoon rainfall. Geophys Res Lett 32:L08704. doi:10.1029/2004GL021979
Krishna Kumar K, Rajagopalan B, Hoerling H, Bates G, Cane M (2006) Unraveling the mystery of Indian monsoon failure during El Niño. Science 314:115–119. doi:10.1126/science.1131152
Krishnan R, Swapna P (2009) Significance influence of the boreal summer monsoon flow on the Indian Ocean response during dipole events. J Clim 22:5611–5634
Krishnan R, Mujumdar M, Vaidya V, Ramesh KV, Satyan V (2003) The abnormal summer monsoon of 2000. J Clim 16:1177–1194
Kucharski F, Bracco A, Yoo JH, Molteni F (2007) Low-frequency variability of the Indian monsoon-ENSO relation and the Tropical Atlantic; the ‘weakening’ of the 1980s and 1990s. J Clim 20:4255–4266
Kucharski F, Bracco A, Yoo JH, Molteni F (2008) Atlantic forced component of the Indian monsoon interannual variability. Geophys Res Lett 35:L04706. doi:10.1029/2007GL033037
Kucharski F, Bracco A, Yoo JH, Tompkins A, Feudale L, Ruti P, Dell’Aquila A (2009) A Gill-Matsuno-type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. Quart J Roy Meteor Soc 135:569–579. doi:10.1002/qj.406
Kulkarni A, Sabade SS, Kripalani RH (2007) Association between extreme monsoons and the dipole mode over the Indian subcontinent. Meteorol Atmos Phys 95:255–268
Li T, Wang B, Chang CP, Zhang YS (2003) A theory for the Indian Ocean dipole-zonal mode. J Atmos Sci 60:2119–2135
Loschnigg J, Meehl GA, Arblaster JM, Compo GP, Webster PJ (2003) The Asian monsoon, the tropospheric biennial oscillation, and the Indian Ocean dipole in the NCAR CSM. J Clim 16:1617–1642
McPhaden MJ, Zhang X (2009) Asymmetry in zonal phase propagation of ENSO sea surface temperature anomalies. Geophys Res Lett 36:L13703. doi:10.1029/2009GL038774
Meehl GA, Arblaster J (2002) The tropospheric biennial oscillation and the Asian-Australian monsoon rainfall. J Climate 15:722–744
Meehl GA, Arblaster JM, Loschnigg J (2003) Coupled Ocean-atmosphere dynamical processes in the tropical Indian and Pacific Oceans and the TBO. J Clim 16:2138–2158
Nicholls N (1995) All-India summer monsoon rainfall and sea surface temperatures around northern Australia and Indonesia. J Clim 8:1463–1467
Nitta T, Yamada S (1989) Recent warming of tropical sea surface temperature and its relationship to the Northern Hemisphere circulation. J Meteor Soc Jpn 67:375–383
Park H-S, Chiang JCH, Lintner BR, Zhang JG (2010) The delayed effect of major El Niño events on Indian monsoon rainfall. J Clim 23:932–946
Parthasarathy B, Munot AA, Kothawale DR (1995) All India monthly and seasonal rainfall series: 1871–1993. Theor Appl Climatol 49:217–224
Peings Y, Douville H, Terray P (2009) Extended winter Pacific North America oscillation as a precursor of the Indian summer monsoon rainfall. Geophys Res Lett 36:L11710. doi:10.1029/2009GL038453
Rajeevan M, Pai DS (2007) On the El Niño-Indian monsoon predictive relationships. Geophys Res Lett 34:L04704. doi:10.1029/2006GL028916
Rajeevan M, Sridhar L (2008) Inter-annual relationship between Atlantic sea surface temperature anomalies and Indian summer monsoon. Geophys Res Lett 35:L21704. doi:10.1029/2008GL036025
Rajeevan M, Pai DS, Anil Kumar R, Lal B (2006) New statistical models for long-range forecasting of southwest monsoon rainfall over India. Clim Dyn. doi:10.1007/s00382-006-0197-6
Rasmusson EM, Carpenter TH (1983) The relationship between the eastern Pacific sea surface temperature and rainfall over India and Sri Lanka. Mon Weather Rev 111:517–528
Ratnam JV, Behera SK, Masumoto Y, Takajashi K, Yamagata T (2010) Pacific Ocean origin for the 2009 Indian summer monsoon failure. Geophys Res Lett 37:L07807. doi:10.1029/2010GL042798
Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res 108(D14):4407. doi:10.1029/2002JD002670
Saji NH, Goswami BN, Vinayachandran PN, Yamagata TA (1999) Dipole mode in the tropical Indian Ocean. Nature 401:360–363
Shukla J (1987) Interannual variability of monsoons in Monsoons. In: Fein JS, Stephens PL (eds), Wiley, Hoboken, pp 399–464
Shukla J, Paolino DA (1983) The southern oscillation and long-range forecasting of the summer monsoon rainfall over India. Mon Wea Rev 111:1830–1837
Slingo JM, Annamalai H (2000) [1997]: The El Niño of the century and the response of the Indian summer monsoon. Mon Wea Rev 128:1778–1797
Sooraj KP, Kug J-S, Li Y, Kang I-S (2009) Impact of El Nino onset timing on the Indian Ocean: Pacific coupling and subsequent El Nino evolution. Theor Appl Climatol 97(1–2):17–27
Srivastava AK, Rajeevan M, Kulkarni R (2002) Teleconnection of OLR and SST anomalies over Atlantic Ocean with Indian summer monsoon. Geophys Res Lett 29:1284. doi:10.1029/2001GL013837
Terray P (1994) An evaluation of climatological data in the Indian Ocean area. J Meteor Soc Japan 72:359–386
Terray P (2010) Southern hemisphere extra-tropical forcing: a new paradigm for El Niño-southern oscillation. Clim Dyn. doi:10.1007/s00382-010-0825-z
Terray P, Dominiak S (2005) Indian Ocean sea surface temperature and El Niño-Southern Oscillation: a new perspective. J Clim 18:1351–1368
Terray P, Delecluse P, Labattu S, Terray L (2003) Sea surface temperature associations with the late Indian summer monsoon. Clim Dyn 21:593–618
Terray P, Dominiak S, Delecluse P (2005) Role of the southern Indian Ocean in the transitions of the monsoon-ENSO system during recent decades. Clim Dyn 24:169–195. doi:10.1007/s00382-004-0480-3
Terray P, Chauvin F, Douville H (2007) Impact of southeast Indian Ocean sea surface temperature anomalies on monsoon-ENSO-dipole variability in a coupled ocean-atmosphere model. Clim Dyn 28:553–580. doi:10.1007/s00382-006-0192-y
Trenberth KE, Caron JM, Stepaniak DP, Worley S (2002) The evolution of ENSO and global atmospheric surface temperatures. J Geophys Res 107(D8). doi:10.1029/2000JD000298
Vimont DJ, Wallace JM, Battisti DS (2003) The seasonal footprinting mechanism in the Pacific: implications for ENSO. J Clim 16:2668–2675
Vimont DJ, Alexander M, Fontaine A (2009) Mid latitude excitation of tropical variability in the pacific: the role of thermodynamic coupling and seasonality. J Clim 22:518–534
Walker GT (1924) Correlation in seasonal variations of weather, IV: a further study of world weather. Mem Ind Meteorol Dep 24:275–332
Wang B (1995) Interdecadal changes in El Niño onset in the last four decades. J Clim 8:267–285
Wang B (2006) The Asian monsoon. Springer/Praxis Publishing, New York, p 787
Wang B, An S-I (2002) A mechanism for decadal changes of ENSO behavior: roles of background wind changes. Clim Dyn 18:475–486
Wang B, Ding Q, Fu X, Kang I-S, Jin K, Shukla J, Doblas-Reyes F (2005) Fundamental challenge in simulation and prediction of summer monsoon rainfall. Geophys Res Lett 32:L15711. doi:10.1029/2005GL022734
Wang B, Yang J, Zhou T (2008) Interdecadal changes in the major modes of Asian–Australian Monsoon variability: strengthening relationship with ENSO since the Late 1970 s. J Clim 21:1771–1788
Webster PJ, Hoyos C (2010) Beyond the spring barrier? Nat Geosci 3:152–153. doi:10.1038/ngeo760
Webster PJ, Yang S (1992) Monsoon and ENSO: selectively interactive systems. Quart J Roy Meteor Soc 118:877–926
Webster PJ, Magana VO, Palmer TN, Shukla J, Tomas RA, Yanai M, Yasunari T (1998) Monsoons: processes, predictability and the prospects for prediction. J Geophys Res 103(C7):14451–14510
Yang J, Liu Q, Xie S-P, Liu Z, Wu L (2007) Impact of the Indian Ocean SST basin mode on the Asian summer monsoon. Geophys Res Lett 34:L02708. doi:10.1029/2006GL028571
Yoo SH, Fasullo J, Yang S, Ho CH (2010) On the relationship between Indian Ocean sea surface temperature and the transition from El Niño to La Niña. J Geophys Res 115:D15114. doi:10.1029/2009JD012978
Zheng X-T, Xie S, Vecchi AG, Liu Q, Hafner J (2010) Indian Ocean dipole response to global warming: analysis of ocean–atmospheric feedbacks in a coupled model. J Clim 23(5). doi:10.1175/2009JCLI3326.1
Acknowledgments
Financial support from the Indo-French CEFIPRA project (N° 3907/1) is acknowledged. The Hadley SST and SLP datasets were provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at URL: http://www.cdc.noaa.gov/. Graphics have been prepared using the SAXO package of Sébastien Masson. We also thank the anonymous reviewers for their comments that improved this paper.
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Boschat, G., Terray, P. & Masson, S. Robustness of SST teleconnections and precursory patterns associated with the Indian summer monsoon. Clim Dyn 38, 2143–2165 (2012). https://doi.org/10.1007/s00382-011-1100-7
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DOI: https://doi.org/10.1007/s00382-011-1100-7