Luo H, Yanai M. 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 , 1984, 112:966 - 989.
[11]
He H Y, McGinnis W, Song Z, et al. Onset of the Asian summer monsoon in 1979 and the effect of the Tibetan Plateau. Mon Wea Rev , 1987, 115: 1966-1995.
[12]
Yanai M, Li C, Song Z. Seasonal heating of the Tibetan Plateau and its effects of the evolution of the Asian summer monsoon. J Meteor Soc Japan, 1992, 70: 319-351.
[13]
Yanai M, Li C. Mechanism of heating and the boundary layer over the Tibetan Plateau. Mon Wea Rev , 1994, 122:305 - 323.
[14]
Wu Guoxiong, Liu Yimin, Mao Jiangyu, et al. 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 of Professor Jijia Zhang, Zhu Xun et al, Eds. World Scientific. 2004, 92- 114.
[15]
Ertel H. Ein neuer hydrodynamische wirbdsatz. Meteorologische Zeitschrift, 1942, 59: 277- 281.
[16]
Hoskins B J. Towards a PV-0 view of the general circulation. Tellus,1990, 43AB: 27- 35.
[17]
Haynes P H, Mclntyre M E. On the evolution of vorticity and potential vorticity in the presents of diabatic heating and friction or other forces. Journal of the Atmospheric Sciences, 1987, 44:828 - 841.
[18]
Haynes P H, Mclntyre M E. On the conservation and impermeability theorems for potential vorticity. Journal of the Atmospheric Sciences,1990, 47:2021 - 2031.
[19]
Wang T A, Lin Y L, Semazzi H F M, et al. Response of stable stratified atmosphere to large-scale diabatic forcing with applications to wind patterns in Brazil and the Sahel. J Geophys Res , 1996,101D3: 7049- 7073.
[20]
Wu Z H. A shallow CISK, deep equilibrium mechanism for the interaction between large-scale convection and large-scale circulation in the tropics. J Atmos Sci , 2003, fill: 377 - 392.
[21]
Zhang X H, Shi G Y, Liu H, et al. lAP Global Ocean-Atmosphere-Land System Model. Beijing, New York: Science Press. 2000, 252.
[22]
Wu T W, Liu P, Wang Z, et al. The performance of atmospheric component model R42L9 of GOALS/LASG. Adv Atmos Sci , 2003,20:726 - 742.
[23]
Liu Y M, Wu G X, Liu H, et al. Condensation heating of the Asian summer monsoon and the subtropical anticyclone in the Eastern Hemisphere. Climate Dynamics, 2001, 17:327-333.
Liu Yimin, Wu Guoxiong, Ren Rongcai. Relationship between the subtropical anticyclone and diabatic heating. J Climate, 2004, 17:682 - 698.
[26]
Wu Guoxiong, Liu Yimin. Summer quadruplet heating pattern in the subtropics and the associated atmospheric circulation. Geophys Res Lett , 2003, 30 (5): 1201, doi: 10. 1029/2002GL016209.
[27]
Duan Anmin, Wu Guoxiong. Role of the Tibetan Plateau thermal forcing in the summer climate patterns over subtropical Asia. Climate Dynamics, 2004 (in press).
