Impact of Indian summer monsoon on the South Asian High and its influence on summer rainfall over China

Climate Dynamics

Volumn 43, Issue 5-6, 2014, Pages 1257-1269

  Wei, Wei ^a,b   Zhang, Renhe ^a   Wen, Min ^a   Rong, Xinyao ^a   Li, Tim ^c  

^a STATE KEY LABORATORY OF SEVERE WEATHER   (China)

^b UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

^c UNIVERSITY OF HAWAII   (United States)

Author keywords

East Asian summer monsoon; Indian summer monsoon; South Asian High; Summer rainfall over China

Indexed keywords

ATMOSPHERIC CIRCULATION; COOLING; HEATING; MONSOON; RAINFALL; SUMMER; TROPOSPHERE;

CHINA; HUAI RIVER; IRANIAN PLATEAU; QINGHAI-XIZANG PLATEAU; YANGTZE VALLEY;

EID: 84906941779     PISSN: 09307575     EISSN: 14320894     Source Type: Journal    
DOI: 10.1007/s00382-013-1938-y     Document Type: Article

References (36)

1. Chen GY, Liao QS (1990) Relationship between the location features of 100 hPa South Asia High and mid-summer rainfall in China. Plateau Meteorol 9: 432-438 (in Chinese).
2. Dai XG, Chou JF, Wu GX (2002) The teleconnection relationship between Indian monsoon and East Asian summer circulation. Acta Meterol Sin 60: 544-552 (in Chinese).
3. Ding Q, Wang B (2005) Circumglobal teleconnection in the Northern Hemisphere summer. J Clim 18: 3483-3505.
4. Guo QY (1992) Teleconnection between the floods/droughts in North China and Indian summer monsoon rainfall. Acta Geogr Sin 47: 394-402 (in Chinese).
5. Hu Z-Z, Wu R, Kinter LJ, Yang S (2005) Connection of summer rainfall variations in South and East Asia: role of El Niño-Southern Oscillation. Int J Climatol 25: 1279-1289.
6. Huang RH (1985) The influence of the heat source anomaly over Tibetan Plateau on the northern hemispheric circulation anomalies. Acta Meteorol Sin 43: 208-219 (in Chinese).
7. Huang Y, Qian YF (2003) Relationship between South Asian High and summer rainfall in North China. Plateau Meteorol 22: 602-607 (in Chinese).
8. Jiang XA, Li T (2005) Reinitiation of the boreal summer intraseasonal oscillation in the tropical Indian Ocean. J Clim 18: 3777-3795.
9. Kripalani RH, Kulkarni A (2001) Monsoon rainfall variations and teleconnections over South and East Asia. Int J Climatol 21: 603-616.
10. Krishnamurti TN, Bhalme H (1976) Oscillations of a monsoon system. Part I. Observational aspects. J Atmos Sci 33: 1937-1954.
11. Krishnamurti TN, Daggupaty SM, Fein J, Kanamitsu M, Lee JD (1973) Tibetan high and upper tropospheric tropical circulation during northern summer. Bull Am Meteor Soc 54: 1234-1249.
12. Li T (2006) Origin of the summertime synoptic-scale wave train in the western North Pacific. J Atmos Sci 63: 1093-1102.
13. Liebmann B, Smith CA (1996) Description of a complete (interpolated) outgoing longwave radiation dataset. Bull Amer Meteor Soc 77: 1275-1277.
14. Liu YY, Ding YH (2008) Analysis and numerical simulation of the teleconnection between Indian summer monsoon and precipitation in North China. Acta Meteorol Sin 66: 789-799 (in Chinese).
15. Liu YM, Wu GX, Liu H, Liu P (1999) The effect of spatially nonuniform heating on the formation and variation of subtropical high part III: condensation heating and South Asia high and western Pacific subtropical high. Acta Meteorol Sin 57: 525-538 (in Chinese).
16. Liu YM, Wu GX, Liu H, Liu P (2001) Condensation heating of the Asian summer monsoon and the subtropical anticyclone in Eastern Hemisphere. Clim Dyn 17: 327-338.
17. Luo H, Yanai M (1984) The large-scale circulation and heat sources over the Tibetan Plateau and surrounding areas during the early summer of 1979. Part II: heat and moisture budgets. Mon Weather Rev 112: 966-989.
18. Luo SW, Qian ZA, Wang QQ (1982) The climatic and synoptical study about the relationship between the Qinghai-Xizang High Pressure on the 100 mb surface and the flood and drought in East China in summer. Plateau Meteorol 1: 1-10 (in Chinese).
19. Luo Y, Zhang R, Qian W, Luo Z, Hu X (2011) Intercomparison of deep convection over the Tibetan Plateau-Asian monsoon region and subtropical North America in boreal summer using CloudSat/CALIPSO data. J Clim 24: 2164-2177.
20. Mason RB, Anderson CE (1963) The development and decay of the 100 mb summertime anticyclone over southern Asia. Mon Weather Rev 91: 3-12.
21. Peixóto JP, Oort AH (1984) Physics of climate. Rev Mod Phys 56: 365-429.
22. Sontakke N, Pant G, Singh N (1993) Construction of all-India summer monsoon rainfall series for the period 1844-1991. J Clim 6: 1807-1811.
23. Tao SY, Chen LX (1987) A review of recent research on the East Asian summer monsoon in China. In: Chang CP, Krishnamurti TN (eds) Monsoon meteorology. Oxford University Press, Oxford, pp 60-92.
24. Tao SY, Zhu FK (1964) The 100-mb flow patterns in southern Asia in summer and its relation to the advance and retreat of the West-Pacific subtropical anticyclone over the Far East. Acta Meteorol Sin 34: 385-396 (in Chinese).
25. Uppala SM, Kållberg PW, Simmons AJ, Andrae U, Bechtold VDC, Fiorino M, Gibson JK, Haseler J, Hernandez A, Kelly GA, Li X, Onogi K, Saarinen S, Sokka N, Allan RP, Andersson E, Arpe K, Balmaseda MA, Beljaars ACM, Berg LVD, Bidlot J, Bormann N, Caires S, Chevallier F, Dethof A, Dragosavac M, Fisher M, Fuentes M, Hagemann S, Hólm E, Hoskins BJ, Isaksen L, Janssen PAEM, Jenne R, McNally AP, Mahfouf JF, Morcrette JJ, Rayner NA, Saunders RW, Simon P, Sterl A, Trenberth KE, Untch A, Vasiljevic D, Viterbo P, Woollen J (2005) The ERA-40 re-analysis. Quart J R Meteor Soc 131: 2961-3012.
26. Wei W, Zhang R, Wen M (2012) Meridional variation of South Asian High and its relationship with the summer precipitation over China. J Appl Meteorol Sci 23: 650-659 (in Chinese).
27. Wu R (2002) A mid-latitude Asian circulation anomaly pattern in boreal summer and its connection with the Indian and East Asian summer monsoon. Int J Climatol 22: 1879-1895.
28. Wu R, Hu Z-Z, Kirtman PB (2003) Evolution of ENSO-related rainfall anomalies in East Asia. J Clim 16: 3742-3758.
29. Wu G, Ren S, Xu J, Wang D, Bao Q, Liu B, Liu Y (2013) Impact of tropical cyclone development on the instability of South Asian High and the summer monsoon onset over Bay of Bengal. Clim Dyn. doi: 10. 1007/s00382-013-1766-0.
30. Yanai M, Esbensen S, Chu J-H (1973) Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets. J Atmos Sci 30: 611-627.
31. Zhang R (1999) The role of Indian summer monsoon water vapor transportation on the summer rainfall anomalies in the northern part of China during the El Niño mature phase. Plateau Meteorol 18: 567-574 (in Chinese).
32. Zhang R (2001) Relations of water vapor transport from Indian monsoon with that over East Asia and the summer rainfall in China. Adv Atmos Sci 18: 1005-1017.
33. Zhang Q, Wu GX (2001) The large area flood and drought over Yangtze River Valley and its relation to the South Asia High. Acta Meteorol Sin 59: 569-577 (in Chinese).
34. Zhang R, Sumi A, Kimoto M (1999) A diagnostic study of the impact of El Niño on the precipitation in China. Adv Atmos Sci 16: 229-241.
35. Zhang Q, Wu GX, Qian YF (2002) The bimodality of the 100 hPa South Asia High and its relationship to the climate anomaly over East Asia in summer. J Meteorol Soc Jpn 80: 733-744.
36. Zuo Z, Zhang R, Zhao P (2011) The relation of vegetation over the Tibetan Plateau to rainfall in China during the boreal summer. Clim Dyn 36: 1207-1219.