Abstract
Previous studies have shown that climate anomalies over the North Atlantic–Europe (NAE) can influence the Indian summer monsoon (ISM) variability. It is, however, still an outstanding question whether the latter has a significant impact on the former. In this study, observational evidences indicate that the interannual variability of ISM is closely linked to the climate anomalies over NAE. A strong ISM is often associated with significant above normal precipitation over most of western Europe. Meanwhile, positive surface air temperature (SAT) anomalies are usually observed over the Mediterranean, accompanied by below normal SAT in Western Europe during a strong ISM summer. The situation is just opposite during a weak ISM summer. A global primitive equation model is utilized to assess the mechanism of the above observed connection.
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References
Ambrizzi T, Hoskins BJ, Hsu HH (1995) Rossby wave propagation and teleconnection patterns in the Austral Winter. J Atmos Sci 52:3661–3672
Bretherton CS, Smith C, Wallace JM (1992) An inter-comparison of methods for finding coupled patterns in climate data. J Clim 5:541–560
Chang CP, Harr P, Ju J (2001) Possible roles of Atlantic circulations on the weakening Indian monsoon-ENSO relationship. J Clim 14:2376–2380
Ding Q, Wang B (2005) Circumglobal teleconnection in the Northern Hemisphere Summer. J Clim 18:3483–3505
Ding Q, Wang B (2007) Intraseasonal teleconnection between the summer European wave train and the Indian monsoon. J Clim 20:3751–3767
Enomoto T, Hoskins BJ, Matsuda Y (2003) The formation mechanism of the Bonin high in August. Q J R Meteorol Soc 129:157–178
Gill AE (1980) Some simple solutions for heat induced tropical circulation. Q J R Meteorol Soc 106:447–462
Goswami BN, Krishnamurthy B, Annamalai H (1999) A broad-scale circulation index for interannual variability of the Indian summer monsoon. Q J R Meteorol Soc 125:611–633
Guo QY, Wang JQ (1988) A comparative study on summer monsoon in China and India (in Chinese). J Trop Meteorol 4:53–60
Hall NMJ (2000) A simple GCM based on dry dynamics and constant forcing. J Atmos Sci 57:1557–1572
Hall NMJ, Derome J (2000) Transients, nonlinearity, and eddy feedback in the remote response to El Niño. J Atmos Sci 57:3992–4007
Held IM, Lyons SW, Nigam S (1989) Transients and the extratropical response to El Nino. J Atmos Sci 46:163–174
Hu ZZ, Latif M, Roeckner E, Bengtsson L (2000) Intensified Asian summer monsoon and its variability in a coupled model forced by increasing greenhouse gas concentrations. Geophys Res Lett 27:2681–2684
Jin FF, Hoskins BJ (1995) The direct response to tropical heating in a baroclinic atmosphere. J Atmos Sci 52:307–319
Kanamitsu M, Ebisuzaki W, Woollen J, Yang SK, Sling JJ, Fiorino M, Potter GL (2002) NCEP-DOE AMIP-II reanalysis (R-2). Bull Am Meteorol Soc 83:1631–1643
Kripalani RH, Kulkarni A (1997) Rainfall variability over Southeast Asia—connections with Indian monsoon and ENSO extremes: New perspective. Int J Climatol 17:1155–1168
Kripalani RH, Kulkarni A (2001) Monsoon rainfall variations and teleconnections over South and East Asia. Int J Climatol 21:603–616
Kripalani RH, Singh SV (1993) Large-scale aspects of India–China summer monsoon rainfall. Adv Atmos Sci 10:72–84
Kumar KK, Rajagopalan B, Cane MA (1999) On the weakening relationship between Indian monsoon and ENSO. Science 284:2156–2159
Lau KM, Weng HY (2002) Recurrent teleconnection patterns linking summertime precipitation variability over East Asia and North America. J Meteorol Soc Jpn 80:1309–1324
Lau KM, Kim KM, Lee JY (2004) Interannual variability, global teleconnection and potential predictability associated with the Asian summer monsoon. In: Chang CP (ed) East Asian monsoon. World Scientific, Singapore, pp 153–172
Liang PD (1988) Indian summer monsoon and rainfall in North China in summer (in Chinese). Acta Meteorol Sin 46:75–81
Liebmann B, Smith CA (1996) Description of a complete (interpolated) outgoing longwave radiation dataset. Bull Am Meteorol Soc 77:1275–1277
Lin H (2009) Global extratropical response to diabatic heating variability of the Asian summer monsoon. J Atmos Sci 66:2697–2713
Lin H, Derome J, Brunet G (2007) The transient atmospheric response to tropical forcing. J Clim 20:5642–5665
Raicich F, Pinardi N, Navarra A (2003) Teleconnections between Indian monsoon and Sahel rainfall and the Mediterranean. Int J Climatol 23:173–186
Rodwell MJ, Hoskins BH (1996) Monsoon and the dynamics of deserts. Q J R Meteorol Soc 122:1385–1404
Rodwell MJ, Jung T (2008) Understanding the local and global impacts of model physics changes: an aerosol example. Q J R Meteorol Soc 134:1479–1497
Sardeshmukh PD, Hoskins BJ (1984) Spatial smoothing on the sphere. Mon Weather Rev 112:2524–2529
Sardeshmukh PD, Hoskins BJ (1988) The generation of global rotational flow by steady idealized tropical divergence. J Atmos Sci 45:1228–1251
Wang B, Wu RG, Lau KM (2001) Interannual variability of the Asian summer monsoon: contrasts between the Indian and the western North Pacific–east Asian monsoons. J Clim 14:4073–4090
Wu ZW, Jiang Z, He J (2006) The comparison analysis of flood and droughts features among the first flood period in South China, Meiyu period in the Yangtze River and Huaihe River valleys and rainy season in north China in the late 50 years (in Chinese). J Atmos Sci 30(3):391–401
Wu ZW, Wang B, Li J, Jin FF (2009) An empirical seasonal prediction model of the East Asian summer monsoon using ENSO and NAO. J Geophys Res 114:D18120. doi:10.1029/2009JD011733
Wu ZW, Li J, Jiang Z, He J, Zhu X (2011) Possible effects of the North Atlantic oscillation on the strengthening relationship between the East Asian Summer monsoon and ENSO. Int J Climatol (in press)
Xie P, Arkin PA (1997) Global precipitation: a 17-year monthly analysis based on gauge observation, satellite estimates, and numerical model outputs. Bull Am Meteorol Soc 78:2539–2558
Acknowledgments
We thank Dr. Ruping Mo and the two reviewers for their helpful comments on the early version of this manuscript. Zhiwei Wu is supported by the Sustainable Agriculture Environment Systems (SAGES) research initiative of Agriculture and Afri-Food Canada through the Natural Sciences and Engineering Research Council of Canada (NSERC) Fellowship Program and the National Basic Research Program “973” (Grant No. 2010CB950400).
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Lin, H., Wu, Z. Indian summer monsoon influence on the climate in the North Atlantic–European region. Clim Dyn 39, 303–311 (2012). https://doi.org/10.1007/s00382-011-1286-8
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DOI: https://doi.org/10.1007/s00382-011-1286-8