No pp The Relationship between Southeast Asian Summer Monsoon and Upper Atmospheric Field over Eurasia Takeshi MORI and Shuji YAMAKAWA
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1 No pp The Relationship between Southeast Asian Summer Monsoon and Upper Atmospheric Field over Eurasia Takeshi MORI and Shuji YAMAKAWA Received September 30, 2006 Using Southeast Asian Summer Monsoon index defined by convection activity in and around the Philippine Sea from 1982 to 2005, the relationship between Southeast Asian Summer monsoon and the upper troposphere to the lower stratosphere over Asia was analyzed. In the strong monsoon years, the tropical easterly jet in the upper layer tends to become strong, and an anomaly wave track which is negative in South Asia and positive in East Asia tends to appear. The statistically significant area of easterly anomaly wind caused by its anomaly wave track reaches the easterly wind area in the stratosphere, to the south of positive geopotential height anomaly over East Asia. Besides, in the nearby upper troposphere to the tropopause, the northward divergence over the Mediterranean region of the subtropical high pressure zone affects activities of the polar jet stream and the Eurasian polar fronts, therefore a positive precipitation anomaly west of Lake Baykal may influence vorticity anomaly over East Asia. Keywords: Southeast Asian Summer Monsoon, the upper troposphere, the lower stratosphere, East Asia, geopotential height anomaly, vorticity anomaly Zhang et al Nitta N PJ 2004 PJ PJEnomoto et al Niwano : : Graduate School of Integrated Basic Sciences, Nihon University: Sakurajosui Setagaya ku, Tokyo, Japan Department of Geosystem Sciences, College of Humanities and Sciences, Nihon University: Sakurajosui Setagaya ku, Tokyo, Japan
2 and Takahashi QBO Terao QBO QBO 2 NCEP/NCAR reanalysis Data P OLR Wang and Fan 1999 convection index N E 6 9 OLR 1 convection index Positive years0.65 Negative years Positive Negative years Negative years years OLR 2 Positive years Negative years Positive years, Negative years OLR ,Takaya and Nakamura 2001 Wave Activity Flux 3 1 convection index convection index2 2 OLR 1 Positive years Negative years 3 Positive years 6 9 Positive years N hPa
3 3 Positive years Positive years N 4 Negative years Positive years N 4 Negative years 6 9 Positive years 3 30 N hPa Negative years Positive years Positive years 2 Positive years 5 Posi- tive years N 6 Positive years N 20 E
4 10 N hPa hPa N 120 E hPa 3 7 Positive years hPa Positive years 200hPa 8 Positive years 6 9 OLR 9 Positive years Positive years hPa P Negative years 200hPa OLR P 11 Positive years hPa hPa 25 N 8 Positive years 6 9 OLR 7 Positive years hPa 9 Positive years
5 hpa 12 Positive years hpa hpa Negative years Positive years 13 Positive years E Positive years E 0 20 N N 25hPa 200hPa 10 Positive years hPa P 12 Positive years hPa 10m/s 11 Positive years hPa 30m/s 13 Positive years E
6 Positive years N Negative years Posi- tive years Positive years20 30 N 60hPa Negative years Positive years E 200hPa Positive years Negative years Positive years Negative years 2004 PJ Positive years PJ Positive years Negative years 14 Positive years hPa Wave Activity Flux 2 m 2 /s Positive years hPa Wave Activity Flux 1 m 2 /s PJ 4 Wave Activity Flux Takaya and Nakamura 2001 Wave Activity Flux 14 Positive years hPa
7 Wave Activity Flux hPa hPa hPa 500hPa 14 PJ 15 Positive years hPa Wave Activity Flux 4 Positive years, Negative years Positive years Negative years 2004 Positive Negative years Negative years years 200hPa Negative years Positive years Positive years Positive years Takaya and Nakamura 2001 Wave Wave Activity FluxPositive years 5 Wave Activity Flux z Positive years
8 Enomoto, T., B. Hoakins and Y. Matsuda 2003The formation mechanism of the Bonin high in August, Q. J. R. Meteorol. Soc, 129, QBO PJ Nitta, T., 1987Convective Activities in the Tropical Western Pacific and Their Impact on the Northern Hemisphere Summer Circulation J. Meteor. Soc. Japan Niwano, M. and M. Takahashi 1998The Influence of Equatorial QBO on the Northern Hemisphere Winter Circulation of a GCM J. Meter. Soc. Japan Takaya, K. and H. Nakamura 2001A Formation of a Phase- Independent Wave-Activity Flux for Stationary and Migratory Quasigeostrophic Eddies on a Zonally Varing Basic Flow, J. Atmos. Sci Terao, T., 1999Relationships between the Quasi-Stationary Rossby Waves in the Subtropical Jet and the Mass and Heat Transport in the Northern Periphery of the Tibetan High J. Meteor. Soc. Japan Wang, B. and Z. Fan 1999Choice of South Asian Summer Monsoon Indies, Bulletin of the American Meteological Society Zhang, Q., G. Wu., Y. Qian 2002The Bimodality of the 100hPa South Asia High and its Relationship to the Climate Anomaly over East Asia in Summer, J.Meter. Soc. Japan
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