Skip to main content

Advertisement

Log in

An Asian–Pacific teleconnection in summer tropospheric temperature and associated Asian climate variability

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

We identified the Asian–Pacific Oscillation (APO) and its associated index, a zonal teleconnection pattern over the extratropical Asian–Pacific region. This was done through the correlation and empirical orthogonal function (EOF) analyses on the summer mean tropospheric eddy temperature from the monthly European Center for Medium-Range Weather Forecast reanalysis. The APO reflects an out-of-phase relationship in variability of the eddy temperature between Asia and the North Pacific and is associated with the out-of-phase relationship in atmospheric heating. The APO index shows a decadal variation, tending to a high-index polarity before 1975 and afterward to a low-index polarity. Moreover, the APO index has a quasi-5-year period. With higher APO-index conditions in the upper troposphere, the summer South Asian high and the North Pacific trough are stronger, while the westerly jet stream over Asia and the easterly jet stream over South Asia strengthen. Also, the Asian low and the North Pacific subtropical high are stronger in the lower troposphere. The anomalous southerlies prevail at the midlatitudes of East Asia, accompanied by a more northward Mei-yu front, and the anomalous westerlies prevail over South Asia. Summer rainfall increases in North China, South China, and South Asia, while it decreases from the valley of the Yangtze River to southern Japan, and near the Philippines.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13

Similar content being viewed by others

References

  • Barnston AG, Livezey RE (1987) Classification, seasonality and persistence of low-frequency atmospheric circulation patterns. Mon Wea Rev 115:1083–1126

    Article  Google Scholar 

  • Chang C-P, Zhang Y-S, Li T (2000) Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part I: roles of the subtropical ridge. J Clim 13:4310–4325

    Article  Google Scholar 

  • Chen L-X, Zhu Q-G, Luo H-B (1991) East Asian monsoons (in Chinese). Chinese Meteorological Press, Beijing, pp 1–362

  • Dao S-Y, Chen L-X (1957) The structure of general circulation over continent of Asia in summer. J Meteor Soc Jpn 75th Ann:215–229

    Google Scholar 

  • Ding H (2004) Seasonal march of the East-Asian summer monsoon. In: Chang C-P (ed) East Asian Monsoon. World Scientific, Singapore, pp 3–53

    Google Scholar 

  • Duan A-M, Wu G-X (2005) Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia. Clim Dyn 24:793–807

    Article  Google Scholar 

  • Flohn H (1957) Large-scale aspects of the “summer monsoon” in South and East Asia. J Meteor Soc Jpn 75th Ann:180–186

    Google Scholar 

  • Gibson JK, Kållberg PW, Uppala S, Hernandez A, Nomura A, Serrano E (1997) ERA description. ECMWF re-analysis project report Series 1, pp 72

  • Hurrell JW (1995) Decadal trends in the North Atlantic oscillation: regional temperature and precipitation. Science 269:676–679

    Article  Google Scholar 

  • Jhun J-G, Lee E-J (2004) A new East Asian winter monsoon index and associated characteristics of the winter monsoon. J Clim 15:711–726

    Article  Google Scholar 

  • Kidson JW (1975) Eigenvector analysis of monthly mean surface data. Mon Wea Rev 103:177–186

    Article  Google Scholar 

  • Krishnamurti TN, Surgi N (1987) Observational aspects of summer monsoon. In: Chang C-P, Krishnamurti TN (eds) Monsoon meteorology. Oxford University Press, New York, pp 3–25

    Google Scholar 

  • Kutzbach JE (1970) Large-scale features of monthly mean Northern Hemisphere anomaly maps of sea-level pressure. Mon Wea Rev 98:708–716

    Article  Google Scholar 

  • Lau K-M (1992) East Asian summer monsoon rainfall variability and climate teleconnection. J Meteor Soc Jpn 70:211–241

    Google Scholar 

  • Lau K-M, Li M-T (1984) The monsoon of East Asia and its global associations—a survey. Bull Am Meteor Soc 65:114–125

    Article  Google Scholar 

  • Lau K-M, Kim K-M, Yang S (2000) Dynamical and boundary forcing characteristics of regional components of the Asian summer monsoon. J Clim 13:2461–2482

    Article  Google Scholar 

  • Li C, Yanai M (1996) The onset and interannual variability of the Asian summer monsoon in relation to land–sea thermal contrast. J Clim 9:358–375

    Article  Google Scholar 

  • Lu E, Chan J-C-L (1999) A unified monsoon index for South China. J Clim 12:2375–2385

    Article  Google Scholar 

  • Luo H-B, Yanai M (1983) The large-scale circulation and heat sources over the Tibetan Plateau and surrounding areas during the early summer of 1979. Part I: Precipitation and kinematic analyses. Mon Wea Rev 111:922–944

    Article  Google Scholar 

  • Luo H-B, 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 Wea Rev 112:966–989

    Article  Google Scholar 

  • Murakami M, Ding H (1982) Wind and temperature changes over Eurasia during the early summer of 1979. J Meteor Soc Jpn 60:183–196

    Google Scholar 

  • Nitta T (1987) Convective activities in the tropical western Pacific and their impacts on the Northern Hemisphere summer circulation. J Meteor Soc Jpn 65:373–390

    Google Scholar 

  • Rodwell MJ, Hoskins BJ (2001) Subtropical anticyclones and summer monsoons. J Clim 14:3192–3211

    Article  Google Scholar 

  • Saji NH, Goswami BN, Vinayachandran, Yamagata T (1999) A dipole mode in the tropical Indian Ocean. Nature 401:360–363

    Google Scholar 

  • Siegert F, Ruecker G, Hinrichs A, Hoffmann AA (2001) Increased damage from fires in logged forests during droughts caused by El Niño. Nature 414:437–440

    Article  Google Scholar 

  • Staff Members of the Section of Synoptic, Dynamic Meteorology, Institute of Geophysics, Meteorology, Academia Sinica, Peking (1957) On the general circulation over eastern Asia (I). Tellus 9:432–446

    Article  Google Scholar 

  • Thompson DWJ, Wallace JM (2001) Regional climate impacts of the Northern Hemisphere annular mode. Science 293:85–89

    Article  Google Scholar 

  • Wallace JM, Gutzler DS (1981) Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon Wea Rev 109:784–812

    Article  Google Scholar 

  • Wang B, Fan Z (1999) Choice of south Asian monsoon indices. Bull Am Meteor Soc 80:629–638

    Article  Google Scholar 

  • Wang B, Wu R-G, Fu X-H (2000) Pacific-east Asian teleconnection: How does ENSO affect Asian climate? J Clim 13:1517–1536

    Article  Google Scholar 

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

    Article  Google Scholar 

  • Yanai M, Li C, Song Z (1992) Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon. J Meteor Soc Jpn 70:319–351

    Google Scholar 

  • Yang S, Lau K-M, Kim K-M (2002) Variations of the East Asian jet stream and Asia–Pacific–American winter climate anomalies. J Clim 15:306–325

    Article  Google Scholar 

  • Ye T-Z, Gao Y-X (1979) The meteorology of the Qinghai-Xizang (Tibet) Plateau (in Chinese). Science Press, Beijing, pp 1–278

  • Zhang P-Q, Yang S, Kousky VE (2005) South Asian high and Asian–Pacific–American climate teleconnection. Adv Atmos Sci 22:915–923

    Article  Google Scholar 

  • Zhao P, Zhou Z-J (2005) East Asian subtropical summer monsoon index and its relationships to rainfall (in Chinese). Acta Meteorol Sin 63:933–941

    Google Scholar 

  • Zhao P, Zhang X-D, Zhou X-J, Ikeda M, Yin Y-H (2004a) The Sea ice extent anomaly in the North Pacific and its impact on the East Asian summer monsoon rainfall. J Clim 17:3434–3447

    Article  Google Scholar 

  • Zhao P, Zhou X-J, Jian Z-M, Sparrow M, Han Y (2004b) Modeling the tropical climate and the impact of the western Pacific sea surface temperature at the Last Glacial Maximum. J Geophys Res 109: D08105. doi:10.1029/2003JD004095

    Article  Google Scholar 

  • Zhao P, Zhang R-H, Liu J-P, Zhou X-J, He J-H (2006) Onset of Southwesterly wind over Eastern China and associated atmospheric circulation and rainfall. Clim Dyn. doi:10.1007/s00382–006–0212-y

Download references

Acknowledgments

We thank the European Center for Medium-Range Weather Forecast for providing reanalysis available on their homepage. This work was jointly sponsored by the National Key Basic Research Project of China (2004CB418302) and the National Natural Science Foundation of China (40625014).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Ping Zhao.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Zhao, P., Zhu, Y. & Zhang, R. An Asian–Pacific teleconnection in summer tropospheric temperature and associated Asian climate variability. Clim Dyn 29, 293–303 (2007). https://doi.org/10.1007/s00382-007-0236-y

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-007-0236-y

Keywords

Navigation