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Advances in Atmospheric Sciences

, Volume 24, Issue 6, pp 1060–1076 | Cite as

Recent progress in the impact of the Tibetan Plateau on climate in China

  • Liu Yimin  (刘屹岷)Email author
  • Bao Qing  (包庆)
  • Duan Anmin  (段安民)
  • Qian Zheng’an  (钱正安)
  • Wu Guoxiong  (吴国雄)
Article

Abstract

Studies of the impacts of the Tibetan Plateau (TP) on climate in China in the last four years are reviewed. It is reported that temperature and precipitation over the TP have increased during recent decades. From satellite data analysis, it is demonstrated that most of the precipitation over the TP is from deep convection clouds. Moreover, the huge TP mechanical forcing and extraordinary elevated thermal forcing impose remarkable impacts upon local circulation and global climate. In winter and spring, stream flow is deflected by a large obstacle and appears as an asymmetric dipole, making East Asia much colder than mid Asia in winter and forming persistent rainfall in late winter and early spring over South China. In late spring, TP heating contributes to the establishment and intensification of the South Asian high and the abrupt seasonal transition of the surrounding circulations. In summer, TP heating in conjunction with the TP air pump cause the deviating stream field to resemble a cyclonic spiral, converging towards and rising over the TP. Therefore, the prominent Asian monsoon climate over East Asia and the dry climate over mid Asia in summer are forced by both TP local forcing and Eurasian continental forcing.

Due to the longer memory of snow and soil moisture, the TP thermal status both in summer and in late winter and spring can influence the variation of Eastern Asian summer rainfall. A combined index using both snow cover over the TP and the ENSO index in winter shows a better seasonal forecast.

On the other hand, strong sensible heating over the Tibetan Plateau in spring contributes significantly to anchor the earliest Asian monsoon being over the eastern Bay of Bengal (BOB) and the western Indochina peninsula. Qualitative prediction of the BOB monsoon onset was attempted by using the sign of meridional temperature gradient in March in the upper troposphere, or at 400 hPa over the TP. It is also demonstrated by a numerical experiment and theoretical study that the heating over the TP leads to a significant variability in the atmospheric circulation on a quasi-biweekly timescale, bearing much similarity to that found from observational studies. Finally, some important issues for further work in understanding the impacts of the TP are raised.

Key words

Tibetan Plateau TP-dipole cyclonic spiral quasi-biweekly oscillation 

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References

  1. Bai, J. Y., X. D. Xu, and S. Q. Yu, 2003a: Summertime deep convection heating over southeast of Tibetan Plateau. Meteorological Science and Technology, 31, 18–22. (in Chinese)Google Scholar
  2. Bai, J. Y., X. D. Xu, Y. S. Zhou, and X. J. Zhang, 2003b: Preliminary research on inhomogeneous distribution of Tibetan Plateau sensible heat fluxes in spring. Journal of Applied Meteorological Science, 14, 363–368. (in Chinese)Google Scholar
  3. Bao, Q., B. Wang, Y. M. Liu, and G. X. Wu, 2007: The impact of the Tibetan Plateau warming on the East Asia Summer Monsoon—An ECHAM model study. Chinese J. Atmo. Sci., in press. (in Chinese)Google Scholar
  4. Bi, Y., X. Li, and Y. F. Qian, 2004: Relation between 300 hPa temperature anomalies over Iranian and Qinghai-Xizang Plateaus and precipitation of China. Plateau Meteorology, 23, 465–471. (in Chinese)Google Scholar
  5. Bian, L., X. Xu, L. Lu, Z. Gao, M. Zhou, and H. Liu, 2003: Analyses of turbulence parameters in the nearsurface layer at Qamdo of the southeastern Tibetan Plateau. Adv. Atmos. Sci., 20(3), 369–378.CrossRefGoogle Scholar
  6. Cai, Y., and Z. A. Qian, 2004: Distribution, changes of atmospheric precipitable water vapor over Qinghai-Xizang Plateau and its surroundings. Plateau Meteorology, 23(1), 1–10. (in Chinese)Google Scholar
  7. Cai, Y., D. L. Li, M. C. Tang, and C. Y. Bai, 2003: Decadal temperature changes over Qinghai-Xizang Plateau in recent 50 years. Plateau Meteorology, 22, 464–470. (in Chinese)Google Scholar
  8. Chen, L. T., 2005: The combined application of snow anomaly over the Tibetan Plateau and ENSO index to the forecast of rainfall in China. Impacts of the Land-Sea Thermal Contrast on the Climate in China, Y. Liu, and Z. Qian, Eds., China Meteorological Press, Beijing, 177–185. (in Chinese)Google Scholar
  9. Chen, L. T., and Z. X. Yan, 1978: A statistical analysis of the influence of anomalous snow cover over Qinghai-Tibetan Plateau during the winter-spring on the monsoon of early summer. Proc. Conf. Medium and Long-Term Hydrometeo rological Prediction in the Basin of the Yangzi River, Vol. I, Hydro-Electric Press, Beijing, 185–194, (in Chinese)Google Scholar
  10. Chen, Y., and Z. C. Li, 2005: diagnostic analysis and numerical simulation on a regional heavy-hard rain in northeast Qinghai-Xizang Plateau. Acta Meteorologica Sinica, 63, 289–300. (in Chinese)Google Scholar
  11. Duan, A. M., and G. X. Wu, 2004: Main heating modes over the Tibetan Plateau in July and the correlation patterns of circulation and precipitation over east Asia. Acta Meteorologica Sinica, 18, 167–178. (in Chinese)Google Scholar
  12. Duan, A. M., and G. X. Wu, 2005: Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia. Climate Dyn., 24, doi:10.1007/s00382-004-0488-8.Google Scholar
  13. Duan, A. M., J. Y. Mao, and G. X. Wu, 2004: Predictability analysis and preliminary application of the Bay of Bengal summer monsoon onset. Plateau Meteorology, 23, 18–25. (in Chinese)Google Scholar
  14. 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 (D), 48(2), 250–257.Google Scholar
  15. Duan, A. M., G. X. Wu, Q. Zhang, and Y. M. Liu, 2006: New proofs of the recent climate warming over the Tibetan Plateau as a result of the increasing greenhouse gases emissions. Chinese Science Bulletin, 51(11), 1396–1400.CrossRefGoogle Scholar
  16. Flohn, H., 1957: Large-scale aspects of the “summer monsoon” in South and East Asia. J. Meteor. Soc. Japan, 75, 180–186.Google Scholar
  17. Fu, Y. F., 2005: The difference of precipitation profiles among Tibetan Plateau, East Asia and tropics. Impacts of the Land-Sea Thermal Contrast on the Climate in China, Y. Liu and Z. Qian, Eds., China Meteorological Press, Beijing, 123–133. (in Chinese)Google Scholar
  18. Fu, Y. F., and Coauthors, 2006: Tower mast of precipitation over the central Tibetan Plateau. Geophys. Res. Lett., 33, L05802, doi:101029/2005G1024713.Google Scholar
  19. Gao, R., Z. G. Wei, W. J. Dong, C. H. Wang, and H. L. Zhong, 2003a: Variation of the snow and frozen soil over Qinghai-Xizang Plateau in the late twentieth century and their relations to climatic change. Plateau Meteorology, 22, 191–196. (in Chinese)Google Scholar
  20. Gao, Z., L. Bian, J. Wang, and L. Lu, 2003b: Discussion on calculation methods of sensible heat flux during GAME/Tibet in 1998. Adv. Atmos. Sci., 20(3), 357–368.CrossRefGoogle Scholar
  21. Gong, Y. F., L. R. Ji, and T. Y. Duan, 2004: Precipitation character of rainy season of Qinghai-Xizang Plateau and onset over east Asia monsoon. Plateau Meteorology, 23, 313–322. (in Chinese)Google Scholar
  22. Gong, Y. F., M. L. Xu, J. H. He, and L. X. Chen, 2006: On the relationship between the eastern Tibet Plateau rainfall and subtropical high shift in summer. Acta Meteorologica Sinica, 64, 90–99. (in Chinese)Google Scholar
  23. Hsu, C. J., and R. A. Plumb, 2000: Nonaxisymmetric thermally driven circulations and upper-tropospheric monsoon dynamics. J. Atmos. Sci., 57, 1255–1276.CrossRefGoogle Scholar
  24. Hsu, H. H., and X. Liu, 2003: Relationship between the Tibetan Plateau heating and East Asian summer monsoon rainfall. Geophys. Res. Lett., 30(20), 2066, doi:10.1029/2003GL017909.CrossRefGoogle Scholar
  25. Huang, R. H., and Coauthors, 2003: Studies on the relationship between the severe climatic disasters in China and the east Asian climate system. Chinese J. Atmos. Sci., 27(4), 770–787. (in Chinese)Google Scholar
  26. Huang, Y. F., and Y. Q. Li, 2003: Analysis of the relationship between winter surface heating in Qinghai-Xizang Plateau and spring air temperature in Sichuan Chongqing Area. Plateau Meteorology, 22, 33–39. (in Chinese)Google Scholar
  27. Jian, A. L., 2003: The impacts of Tibetan Plateau on the climate of tropical China and on the cultivation of rubber tree. Tropical Geography, 23, 199–203. (in Chinese)Google Scholar
  28. 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 and the western Pacific warm pool. Journal of Tropical Meteorology, 20, 355–364. (in Chinese)Google Scholar
  29. Jiang, H, G. D. Cheng, and K. L. Wang, 2006: Analyzing and measuring the surface temperature of Qinghai-Tibet Plateau. Chinese Journal of Geophysics, 49(2), 391–397. (in Chinese)Google Scholar
  30. Krishnamurti, T. N., and H. N. Bhalme, 1976: Oscillations of a monsoon system. Part I. Observational aspects. J. Atmos. Sci., 33, 1937–1954.CrossRefGoogle Scholar
  31. Li, D. L., W. Li, W. J. Li, L. Z. Lü, H. L. Zhong, and G. L. Ji, 2003a: The effect of surface sensible heat flux of the Qinghai-Xizang Plateau on general circulation over the Northern Hemisphere and climatic anomaly of China. Climatic and Environmental Research, 8, 60–70. (in Chinese)CrossRefGoogle Scholar
  32. Li, D. L., W. J. Li, W. Li, H. L. Zhong, L. Z. Lü, and G. L. Ji, 2003b: A diagnostic study of surface sensible heat flux anomaly over the Qinghai-Xizang Plateau. Climatic and Environmental Research, 8, 71–83. (in Chinese)Google Scholar
  33. Li, D. L., H. L. Zhong, W. Li, and L. Z. Lu, 2004: The abnormal sand-dust storm in Northern China during spring and its response to surface sensible heat on Qinghai-Xizang Plateau in winter. Journal of Arid Land Resources and Environment, 18, 45–51. (in Chinese)Google Scholar
  34. Li, D. L., H. L. Zhong, Q. B. Wu, Y. J. Zhang, Y. L. Hou, and M. C. Tang, 2006a: Analyses on changes of surface temperature over Qinghai-Xizang Plateau. Plateau Meteorology, 24, 291–298. (in Chinese)Google Scholar
  35. Li, G. P., T. Y. Duan, and G. F. Wu, 2003c: The intensity of surface heat source and surface heat balance on the western Qinghai-Xizang plateau. Scientia Geographica Sinica, 23, 13–18 (in Chinese)Google Scholar
  36. Li, S. C., L. Xu, Y. X. Guo, W. H. Qian, G. Q. Zhang, and C. Li, 2006b: Change of annual air temperature over Qingha-Tibet Plateau during recent 34 years. Journal of Desert Research, 26, 27–34. (in Chinese)Google Scholar
  37. Li, S. M., and Coauthors, 2006c: Analyses of ABL structure and interaction of near surface in Mt Qomolangma region. Plateau Meteorology, 25(5), 807–813. (in Chinese)Google Scholar
  38. Li, Y. Q., 2003: Surface heating in the Tibetan Plateau and general circulation over it and their relations with the prediction of drought-flood at its eastern side. Chinese J. Atmos. Sci., 27, 107–114. (in Chinese)Google Scholar
  39. Liang, X. Y., Y. M. Liu, and G. X. Wu, 2005a: The impact of Qinghai-Xizang Plateau uplift on Asian general circulation in spring and summer. Plateau Meteorology, 24, 837–845. (in Chinese)Google Scholar
  40. Liang, X. Y., Y. M. Liu, and G. X. Wu, 2005b: Effect of Tibetan Plateau on the site of onset and intensity of the asian summer monsoon. Acta Meteorologica Sinica, 63, 799–805. (in Chinese)Google Scholar
  41. Liang, X. Y., Y. M. Liu, and G. X. Wu, 2006: Roles of tropical and subtropical land-sea distribution and the Qinghai-Xizang Plateau in the formation of the Asian summer monsoon. Chinese Journal of Geophysics, 49(4), 983–992. (in Chinese)Google Scholar
  42. Liu, H., H. Zhong, L. Bian, J. Chen, M. Zhou, X. Xu, S. Li, and Y. Zhao, 2002a: Characteristics of the micrometeorology in the surface layer in the Tibetan Plateau. Adv. Atmos. Sci., 19(1), 73–88.CrossRefGoogle Scholar
  43. Liu, H. Q., Z. B. Sun, and W. J. Zhu, 2003: Interdecadal relation between snow cover over the Tibetan Plateau and Asian monsoon circulation. Journal of Nanjing Institute of Meteorology, 26, 733–739. (in Chinese)Google Scholar
  44. Liu, X. R., and G. P. Li, 2006: Review and prospect of research on the Tibetan Plateau vortex. Arid Meteorology, 24, 60–66. (in Chinese)Google Scholar
  45. Liu, Y. M., J. C. L. Chan, J. Y. Mao, and G. X. Wu, 2002b: The role of Bay of Bengal convection in the onset of the 1998 South China Sea Summer Monsoon. Mon. Wea. Rev., 130, 2731–2744.CrossRefGoogle Scholar
  46. Liu, Y. M., G. X. Wu, and R. C. Ren, 2004: Relationship between the subtropical anticyclone and diabatic heating. J. Climate, 17, 682–698.CrossRefGoogle Scholar
  47. Liu, Y. M., B. J. Hoskins, and M. Blackburn, 2007: Impact of Tibetan Orography and Heating on the Summer Flow over Asia. J. Meteor. Soc. Japan, 85B, 1–19.CrossRefGoogle Scholar
  48. Lu, J. H., G. P. Li, L. Shi, L. P. Hao, and L. R. Zhou, 2003: Correlation research between low-pressure systems on the east side of Qinghai-Xizang Plateau and snow cover over Plateau. Plateau Meteorology, 22, 121–126. (in Chinese)Google Scholar
  49. Ma, X. B., and Z. Y. Hu, 2005: Precipitation variation characteristics and abrupt change over Qinhai-Xizang Plateau in recent 40 years. Journal of Desert Research, 25, 137–139. (in Chinese)Google Scholar
  50. Ma, Y., H. Ishikawa, O. Tsukamoto, M. Menenti, Z. Su, T. Yao, T. Koike, and T. Yasunari, 2003: Regionalization of surface fluxes over heterogeneous landscape of the Tibetan Plateau by using satellite remote sensing. J. Meteor. Soc. Japan., 81, 277–293.CrossRefGoogle Scholar
  51. Ma, Y. M., T. D. Yao, and J. M. Wan, 2006a: Experimental study of energy and water cycle in Tibetan Plateau—The progress introduction on the study of GAME/Tibet and CAMP/Tibet. Plateau Meteorology, 25, 344–351. (in Chinese)Google Scholar
  52. Ma, Y., L. Zhong, Z. Su, H. Ishikawa, M. Menenti, and T. Koike, 2006b: Determination of regional distributions and seasonal variations of land surface heat fluxes from Landsat-7 Ehanced Thematic Mapper data over the central Tibetan Plateau area. J. Geophys. Res., D10305, doi:10.1029/2005JD006742.Google Scholar
  53. Mao, J. Y., and A. M. Duan, 2005: The predictability of the reversal of the ridge of the subtropical anticyclone and the onset of the summer Asian Monsoon. Impacts of the Land-Sea Thermal Contrast on the Climate in China, Liu Y. and Z. Qian, Eds., China Meteorological Press, Beijing, 173–177. (in Chinese)Google Scholar
  54. Mao, J. Y., G. X. Wu, and Y. M. Liu, 2002a: Study on modal variation of subtropical high and its mechanism during seasonal transition part I: Climatological features of subtropical high structure. Acta Meteorologica Sinica, 60(4), 400–408. (in Chinese)Google Scholar
  55. Mao, J. Y., G. X. Wu, and Y. M. Liu, 2002b: Study on modal variation of subtropical high and its mechanism during seasonal transition part II: Seasonal transition index over Asian Monsoon Region. Acta Meteorologica Sinica, 60(4), 409–420. (in Chinese)Google Scholar
  56. Nan, Z. T., S. X. Li, and G. D. Cheng, 2005: Prediction of permafrost distribution on the Qinghai-Tibet Plateau in the next 50 and 100 years. Science in China, Series D: Earth Sciences, 48(6), 797–804. (in Chinese)CrossRefGoogle Scholar
  57. Ning, L., and Y. F. Qian, 2006: Oscillation characteristics of sensible heat in north Africa and Qinghai-Xizang Plateau and their impacts on the rainfall in east China. Plateau Meteorology, 25, 357–365. (in Chinese)Google Scholar
  58. Peng, J. B., L. T. Chen, and Q. Y. Zhang, 2005a: Multiscale variations of snow cover over QXP and Tropical Pacific SST and their influences on summer rainfall in China. Plateau Meteorology, 24, 366–377. (in Chinese)Google Scholar
  59. Peng, Y., and Coauthors, 2005b: Characteristics of micro-meteorology in the surface layer over Tibetan Plateau area. Universitatis Pekinensis (Acta Scientiarum Naturalism), 41, 180–190. (in Chinese)Google Scholar
  60. Qian, Y. F., Y. Zhang, and Y. Q. Zheng, 2003: Impacts of the Tibetan Plateau snow anomaly in winter and spring on precipitation in China in spring and summer. Arid Meteorology, 21, 1–7. (in Chinese)Google Scholar
  61. Qian, Z. A., T. W. Wu, and X. Y. Liang, 2001: Feature of mean vertical circulation over the QXP and its Neighborhood. Chinese J. Atmos. Sci., 25(3), 237–249. (in Chinese)Google Scholar
  62. Queney, P., 1948: The problem of air flow over mountains: A summary of theoretical studies. Bull. Amer. Meteor. Soc., 29, 16–29.Google Scholar
  63. Tao, S. Y., and F. K. Zhu, 1964: The variation of 100 mb circulation over south Asia in summer and its association with arch and withdraw of west pacific Subtropical High. Acta Meteorologica Sinica, 34, 385–395. (in Chinese)Google Scholar
  64. Tao, S. Y., L. S. Chen, and X. D. Xu, and Y. S. Xiao, 2000a: Progresses of Theoretical Study in the Second Tibetan Plateau Atmosphere Scientific Experiment. Part I. China Meteorological Press, Beijing, 348pp. (in Chinese)Google Scholar
  65. Tao, S. Y., L. S. Chen, and X. D. Xu, and Y. S. Xiao, 2000b: Progresses of Theoretical Study in the Second Tibetan Plateau Atmosphere Scientific Experiment. Part II. China Meteorological Press, Beijing, 396pp. (in Chinese)Google Scholar
  66. Tao, S. Y., L. S. Chen, and X. D. Xu, and G. C. Zhang, 2000c: Progresses of Theoretical Study in the Second Tibetan Plateau Atmosphere Scientific Experiment. Part III. China Meteorological Press, Beijing, 203pp. (in Chinese)Google Scholar
  67. Tian, S. F., and T. Yasunari, 1992: Time and space structure of interannual variations in summer rainfall over China. J. Meteor. Soc. Japan, 70, 585–596.Google Scholar
  68. Wan, R. J., and G. X. Wu, 2007: Mechanism of the Spring Persistent Rains over southeastern China. Sciences in China (D), 50, 130–144CrossRefGoogle Scholar
  69. Wang, C. H., D. W. Jie, and Z. G. Wei, 2003a: Study on relationship between the frozen thaw process in Qinghai-Xizang Plateau and circulation in east-Asia. Chinese Journal of Geophysics, 46, 309–316. (in Chinese)Google Scholar
  70. Wang, L. N., Q. L. Zheng, and Q. L. Song, 2003b: Numerical simulation of the influences of west central Qinghai-Xizang Plateau on East Asia seasonal transition. Plateau Meteorology, 22, 179–184. (in Chinese)Google Scholar
  71. Wang, Z. Z., G. X. Wu, T. W. Wu, and R. C. Yu, 2004: Simulation of the seasonal variations od Asian monsoon with the climate model R42L9/LASG. Adv. Atmos. Sci., 21, 879–889Google Scholar
  72. Wei, L., and D. L. Li, 2003: Evaluation of NCEP/PDOE surface flux data over Qinghai-Xizang Plateau. Plateau Meteorology, 5, 478–487. (in Chinese)Google Scholar
  73. Wei, Z. G., R. H. Huang, and W. J. Dong, 2003: Interannual and interdecadal variations of air temperature and precipitation over the Tibetan Plateau. Chinese J. Atmos. Sci., 27, 157–170. (in Chinese)Google Scholar
  74. Wei, Z., R. H. Huang, and W. Chen, 2005: The Causes of the interannual variation of snow cover over the Tibetan Plateau. Journal of Glaciology and Geocryology, 27, 491–497. (in Chinese)Google Scholar
  75. Wu, G. X., 2004: Recent advances in QXP climate dynamic research. Quarterly Science, 24(1), 1–9. (in Chinese)Google Scholar
  76. Wu, G. X., and 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.CrossRefGoogle Scholar
  77. Wu, G. X., and Y. M. Liu, 2003: Summertime quadruplet heating pattern in the subtropics and the associated atmospheric circulation. Geophys. Res. Lett., 30(5), 1201, doi:10.1029/2002GL016209.CrossRefGoogle Scholar
  78. Wu, G. X., W. P. Li, and H. Guo, 1997: Tibetan Plateau sensible heat pump and Asia summer monsoon. Memorial Corpus for Zhao Jiuzhang, Ye Duzheng, Ed., Science Press, Beijing, 116–126. (in Chinese)Google Scholar
  79. Wu, G. X., Y. M. Liu, and J. Y. Mao, 2004: Adaptation of the atmospheric circulation to thermal forcing over the Tibetan Plateau: Observation, theory and modeling of the atmospheric variability. Selected Papers of Nanjing Institute of Meteorology Alumni in Commemoration for Professor Zhang Ji-ja, Xun Zhu et al., Eds. World Scientific, 92–114.Google Scholar
  80. Wu, G. X., J. Wang, X. Liu, and Y. M. Liu, 2005a: Numerical modeling of the influence of Eurasian orography on the atmospheric circulation in different seasons. Acta Meteorologica Sinica, 63(5), 603–612. (in Chinese)Google Scholar
  81. Wu, G. X., Y. M. Liu, X. Liu, A. M. Duan, and X. Y. Liang, 2005b: How the heating over the Tibetan Plateau affects the Asian climate in summer. Chinese J. Atmos. Sci., 29, 47–56. (in Chinese)Google Scholar
  82. Wu, G. X., and Coauthors, 2007: The Influence of the Mechanical and Thermal Forcing of the Tibetan Plateau on the Asian Climate. Journal of Hydrometeorology, 8, in press.Google Scholar
  83. Wu, S. H., Y. H. Yin, D. Zheng, and Q. Y. Yang, 2005c: Climate changes in the Tibetan Plateau during the last 3 decades. Acta Geographica Sinica, 60, 3–11. (in Chinese)Google Scholar
  84. Wu, T. W., and Z. A. Qian, 2000: Further studies of relation between QXP winter and spring snow anomaly and east China summer precipitation. Acta Meteorologica Sinica, 58(5), 570–581. (in Chinese)Google Scholar
  85. Wu, T. W., and Z. A. Qian, 2003: The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall: An observation investigation. J. Climate, 16, 2038–2051.CrossRefGoogle Scholar
  86. Xu, X. K., H. Chen, and G. Q. Zhou, 2005: The spatiotemporal distribution of land surface features in the Tibetan Plateau. Climatic and Environmental Research, 10, 409–420. (in Chinese)Google Scholar
  87. Yanai, M., and G. X. Wu, 2006: Effects of the Tibetan Plateau. The Asian Monsoon, B. Wang, Ed., Springer, 513–549.Google Scholar
  88. Yanai, M., S. Esbensen, and J.-H. Chu, 1973: Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets. J. Atmos. Sci., 30, 611–627.CrossRefGoogle Scholar
  89. Yeh, T. C., and Y. X. Gao, 1979: Qinghai-Xizang Plateau Meteorology. Science Press, Beijing, 1–278. (in Chinese)Google Scholar
  90. 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)Google Scholar
  91. Yeh, T. C., and Coauthors, 1958: Abrupt phenomenon of general circulation in June and October. Acta Meteorologica Sinica, 29, 249–263. (in Chinese)Google Scholar
  92. Yu, J. H., J. Liu, and Y. Ding, 2004: Annual and diurnal variations of surface fluxes in western Qinghai-Xizang Plateau. Plateau Meteorology, 23, 353–359. (in Chinese)Google Scholar
  93. Zhang, J. J., B. Z. Zhu, and F. K. Zhu, 1988: Tibetan Plateau Meteorological Progresses. Science Press, Beijing, 268pp. (in Chinese)Google Scholar
  94. Zhang, Q. Y., Z. H. Jin, and J. B. Peng, 2006: The relationship between convection over the Tibetan Plateau and circulation over East Asia. Chinese J. Atmos. Sci., 30, 802–812. (in Chinese)Google Scholar
  95. Zhang, S. L., and S. Y. Tao, 2001: Diagnostic and numerical studies on the impacts of Qinghai-Xizang Plateau snow cover on Asian monsoon. Chinese J. Atmos. Sci., 25, 372–390. (in Chinese)Google Scholar
  96. Zhao, P., and L. X. Chen, 2001: Climatic features of atmospheric heat source over the Qinghai-Xizang (Tibetan) Plateau in 35 years and its relation to rainfall in China. Science in China (Series D), 31, 858–864.Google Scholar
  97. Zhao, P., Z. J. Zhou, and J. P. Liu, 2007: Variability of Tibetan spring snow and its associations with the hemispheric extra-tropical circulation and East Asian summer monsoon rainfall: An observational investigation. J. Climate, 20, 3942–3955.CrossRefGoogle Scholar
  98. Zhao, S. R., Z. S. Song, and L. R. Ji, 2003: Heating effect of the Tibetan Plateau on rainfall anomalies over north china during rainy season. Chinese J. Atmos. Sci., 27, 883–893. (in Chinese)Google Scholar
  99. Zhong, H. L., D. L. Li, and W. Li, 2004: The abnormal sand-dust storm in northern China during spring and its response to surface sensible heat on Qinghai-Xizang Plateau in winter. Journal of Desert Research, 24, 323–329. (in Chinese)Google Scholar
  100. Zhou, M. Y., and Coauthors, 2000: The Observation, Diagnosis and Dynamics of the Atmospheric Boundary over the Tibetan Plateau. Meteorological Press, Beijing, 125pp. (in Chinese)Google Scholar
  101. Zuo, H. C., Y. Hu, D. Li, S. Lu and Y. Ma, 2005: Seasonal transition and its boundary layer characteristics in Amdo area of Tibetan Plateau. Progress In Natural Science, 15(3), 239–245.CrossRefGoogle Scholar

Copyright information

© Science Press 2007

Authors and Affiliations

  • Liu Yimin  (刘屹岷)
    • 1
    Email author
  • Bao Qing  (包庆)
    • 1
  • Duan Anmin  (段安民)
    • 1
  • Qian Zheng’an  (钱正安)
    • 2
  • Wu Guoxiong  (吴国雄)
    • 1
  1. 1.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  2. 2.Cold and Arid Regions Environmental and Engineering Research InstituteChinese Academy of SciencesLanzhouChina

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