Chen L. X., F. Schmidt, and W. Li, 2003: Characteristics of the atmospheric heat source and moisture sink over the Qinghai-Tibetan Plateau during the second TIPEX of summer 1998 and their impact on surrounding monsoon. Meteor. Atmos. Phys., 83( 1-2), 1- 18.http://link.springer.com/article/10.1007/s00703-002-0546-x
Chen P., M. P. Hoerling, and R. M. Dole, 2001: The origin of the subtropical anticyclones. J. Atmos. Sci., 58, 1827- 1835.http://adsabs.harvard.edu/abs/2001JAtS...58.1827C
Cui Y. F., A. M. Duan, Y. M. Liu, and G. X. Wu, 2015: Interannual variability of the spring atmospheric heat source over the Tibetan Plateau forced by the North Atlantic SSTA. Climate Dyn., 45, 1617- 1634.http://onlinelibrary.wiley.com/resolve/reference/XREF?id=10.1007/s00382-014-2417-9
Dee, D. P., Coauthors, 2011: The ERA-interim reanalysis: Configuration and performance of the data assimilation system.Quart. J. Roy. Meteor. Soc., 137, 553- 597.http://onlinelibrary.wiley.com/doi/10.1002/qj.828/full
Duan A. M., G. X. Wu, 2005: Role of the Tibetan plateau thermal forcing in the summer climate patterns over subtropical Asia. Climate Dyn., 24, 793- 807.http://link.springer.com/10.1007/s00382-004-0488-8
Duan A. M., G. X. Wu, 2008: Weakening trend in the atmospheric heat source over the Tibetan Plateau during recent decades. Part I: Observations. J.Climate, 21, 3149- 3164.http://nsr.oxfordjournals.org/external-ref?access_num=10.1175/2007JCLI1912.1&link_type=DOI
Duan A. M., Y. M. Liu, and G. X. Wu, 2005: Heating status of the Tibetan Plateau from April to June and rainfall and atmospheric circulation anomaly over East Asia in midsummer. Science in China Series D: Earth Sciences, 48, 250- 257.http://d.wanfangdata.com.cn/Periodical/zgkx-ed200502012
Duan A. M., G. X. Wu, and X. Y. Liang, 2008: Influence of the Tibetan Plateau on the summer climate patterns over Asia in the IAP/LASG SAMIL model. Adv. Atmos. Sci.,25, 518-528, doi: 10.1007/s00376-008-0518-2.http://d.wanfangdata.com.cn/Periodical_dqkxjz-e200804002.aspx
Duan A. M., M. R. Wang, Y. H. Lei, and Y. F. Cui, 2013: Trends in summer rainfall over China associated with the Tibetan Plateau sensible heat source during 1980-2008. J.Climate, 26, 261- 275.http://nsr.oxfordjournals.org/external-ref?access_num=10.1175/JCLI-D-11-00669.1&link_type=DOI
Flohn H., 1957: Large-scale aspects of the "summer monsoon" in South and East Asia. J. Meteor. Soc.Japan, 75, 180- 186.http://ci.nii.ac.jp/naid/10014595971/
Gill A. E., 1980: Some simple solutions for heat-induced tropical circulation.Quart. J. Roy. Meteor. Soc., 106, 447- 462.http://onlinelibrary.wiley.com/doi/10.1002/qj.49710644905/full
He B., S. Yang, and Z. N. Li, 2016: Role of atmospheric heating over the South China Sea and western Pacific regions in modulating Asian summer climate under the global warming background. Climate Dyn.,46, 2897-2908, doi: 10.1007/s00382-015-2739-2.http://link.springer.com/10.1007/s00382-015-2739-2
Jian M. Q., H. B. Luo, and Y. T. Qiao, 2004: On the relationships between the summer rainfall in China and the atmospheric heat sources over the eastern Tibetan Plateau and the western pacific warm pool. Journal of Tropical Meteorology, 10, 133- 143.http://d.wanfangdata.com.cn/Periodical/rdqxxb-e200402003
Krishnamurti T. N., S. M. Daggupaty, J. Fein, M. Kanamitsu, and J. D. Lee, 1973: Tibetan High and upper tropospheric tropical circulation during Northern summer. Bull. Amer. Meteor. Soc., 54, 1234- 1249.
Li J. N., W. G. Meng, A. Y. Wang, L. M. Liu, R. Q. Feng, and E. B. Hou, 2003: Climatic characteristics of the intensity and position of the subtropical high in the western pacific. Tropical Geography, 23( 1), 35- 39. (in Chinese)http://en.cnki.com.cn/article_en/cjfdtotal-rddd200301008.htm
Liu Y. M., G. X. Wu, 2004: Progress in the study on the formation of the summertime subtropical anticyclone. Adv. Atmos. Sci.,21(3), 322-342, doi: 10.1007/BF02915562.http://d.wanfangdata.com.cn/Periodical_dqkxjz-e200403003.aspx
Liu Y. M., G. X. Wu, H. Liu, and P. Liu, 2001: Condensation heating of the Asian summer monsoon and the subtropical anticyclone in the Eastern Hemisphere. Climate Dyn., 17, 327- 338.http://link.springer.com/article/10.1007/s003820000117
Luo H. B., M. Yanai, 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.http://adsabs.harvard.edu/abs/1984MWRv..112..966L
Peng G., M. Domrös, 1987: Connections of the west Pacific subtropical high and some hydroclimatic regimes in China with Antarctic ice-snow indices. Meteor. Atmos. Phys., 37, 61- 71.http://link.springer.com/article/10.1007/BF01040839
Rayner N. A., D. E. Parker, E. B. Horton, C. K. Folland , L. V. Alexand er, D. P. Rowell, E. C. Kent, and A. Kaplan, 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.http://onlinelibrary.wiley.com/doi/10.1029/2002JD002670/full
Rodwell M. J., B. J. Hoskins, 2001: Subtropical anticyclones and summer monsoons. J.Climate, 14, 3192- 3211.http://adsabs.harvard.edu/abs/2001JCli...14.3192R
Wang B., R. G. Wu, and X. H. Fu, 2000: Pacific-East Asian teleconnection: How does ENSO affect East Asian climate? J.Climate, 13, 1517- 1536.http://xueshu.baidu.com/s?wd=paperuri%3A%28c25afe041658a4f704de554223c4d38e%29&filter=sc_long_sign&tn=SE_xueshusource_2kduw22v&sc_vurl=http%3A%2F%2Fwww.bioone.org%2Fservlet%2Flinkout%3Fsuffix%3Di1551-5036-22-3-625-Wang1%26dbid%3D16%26doi%3D10.2112%252F04-0156.1%26key%3D10.1175%252F1520-0442%282000%290132.0.CO%253B2&ie=utf-8&sc_us=573464951031400502
Wang C. L., L. Zou, 2004: West pacific subtropical high's interannual variability and relativity to ENSO. Journal of Tropical Meteorology, 20( 2), 137- 144. (in Chinese)http://en.cnki.com.cn/Article_en/CJFDTOTAL-RDQX200402003.htm
Wang Z. Q., A. M. Duan, and G. X. Wu, 2014: Time-lagged impact of spring sensible heat over the Tibetan Plateau on the summer rainfall anomaly in East China: Case studies using the WRF model. Climate Dyn., 42, 2885- 2898.http://adsabs.harvard.edu/abs/2014AGUFMPP43D1502D
Wu G. X., Y. S. Zhang, 1998: Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea. Mon. Wea. Rev., 126, 913- 927.http://adsabs.harvard.edu/abs/1998MWRv..126..913W
Wu G. X., Y. M. Liu, 2003: Summertime quadruplet heating pattern in the subtropics and the associated atmospheric circulation. Geophys. Res. Lett.,30, doi: 10.1029/2002GL016209.http://onlinelibrary.wiley.com/doi/10.1029/2002GL016209/full
Wu G. X., W. P. Li, and H. Liu, 1997: Sensible heating-driving air pump of the Tibetan Plateau and the Asian summer monsoon. Memorial Volume of Prof, J. Z. Zhao and D. Z. Ye, Eds., Science Press, Beijing, 116- 126. (in Chinese)
Wu G. X., Y. M. Liu., and P. Liu, 1999: The effect of spatially nonuniform heating on the formation and variation of subtropical high I. Scale analysis. Acta Meteorologica Sinica, 57( 3), 257- 263. (in Chinese)
Wu B., T. J. Zhou, and T. Li, 2009: Contrast of rainfall-SST relationships in the Western North Pacific between the ENSO-developing and ENSO-decaying summers. J.Climate, 22, 4398- 4405.http://www.cabdirect.org/abstracts/20093252197.html
Wu B., T. Li, and T. J. Zhou, 2010a: Relative contributions of the Indian Ocean and local SST anomalies to the maintenance of the western North Pacific anomalous anticyclone during the El Niño decaying summer. J.Climate, 23, 2974- 2986.http://www.cabdirect.org/abstracts/20103214989.html
Wu B., T. Li, and T. J. Zhou, 2010b: Asymmetry of atmospheric circulation anomalies over the Western North Pacific between El Niño and La Niña. J.Climate, 23, 4807- 4822.http://www.cabdirect.org/abstracts/20103330883.html
Xie S. P., K. M. Hu, J. Hafner, H. Tokinaga, Y. Du, G. Huang, and T. Sampe, 2009: Indian Ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño. J.Climate, 22, 730- 747.http://www.cabdirect.org/abstracts/20093117314.html
Yang J. L., Q. Y. Liu, S. P. Xie, Z. Y. Liu, and L. X. Wu, 2007: Impact of the Indian Ocean SST basin mode on the Asian summer monsoon. Geophys. Res. Lett.,34, doi: 10.1029/2006GL028571.http://onlinelibrary.wiley.com/doi/10.1029/2006GL028571/full
Ye D. Z., G. X. Wu, 1998: The role of the heat source of the Tibetan Plateau in the general circulation. Meteor. Atmos. Phys., 67, 181- 198.http://link.springer.com/article/10.1007/BF01277509
Yeh T. C., Y. X. Gao, 1979: Meteorology of the Qinghai-Xizang (Tibet) Plateau. Science Press, Beijing, 278 pp. (in Chinese)
Yeh T. C., S. W. Lo, and P. C. Chu, 1957: The wind structure and heat balance in the lower troposphere over Tibetan Plateau and its surrounding. Acta Meteorologica Sinica, 28, 108- 121. (in Chinese)http://en.cnki.com.cn/Article_en/CJFDTotal-QXXB195702002.htm
Zhang R., H. S. Shi, and S. H. Yu, 1995: A study of non-linear stability of the western-Pacific subtropical high. Scientia Atmospherica Sinica, 19, 687- 700. (in Chinese)
Zhang R. H., A. Sumi, 2002: Moisture circulation over East Asia during El Niño episode in northern winter, spring and autumn. J. Meteor. Soc.Japan, 80, 213- 227.http://ci.nii.ac.jp/naid/110001807731
Zhao P., L. X. Chen, 2001: Climatic features of atmospheric heat source/sink over the Qinghai-Xizang Plateau in 35 years and its relation to rainfall in China. Science in China Series D: Earth Sciences, 44, 858- 864.http://d.wanfangdata.com.cn/Periodical_zgkx-ed200109010.aspx