SUBTROPICAL HIGH, LATENT HEATING BY CONVECTION AND ASSOCIATION WITH DISSIPATION AND MAINTENANCE OF SOUTH CHINA SEA TYPHOONSI

[1]	Anthes R A, Hsie E Y, Kuo Y H, 1987. Description of the Penn State/NCAR Mesoscale Model Version 4 (MM4), NCAR Tech. Note, NCAR/TN-282-STR, 66.
[2]	Dietachmayer G S, Droegemeier K K, 1992. Application of continuous dynamic grid adoption techniques to meteorological modeling. Part I: Basic formulation and accuracy. Mon. Wea. Rev., 1992. 120: 1675-1706.
[3]	Dietachmayer G S, Droegemeier K K, 1992. Application of continuous dynamic grid adoption techniques to meteorological modeling. Part Ⅱ: Efficiency. Mon. Wea. Rev., 1992. 120: 1707-1722.
[4]	Li Shenshen, Shou Shouwen, Wang Xin, 1992. Interactions between landing typhoon and heavy rain in the peripheral (in Chinese). Acta aleteor. Sin.50: 35-40.
[5]	Tan banning, Shen Tongli, Ding Yihui et al., Design of auto-adaptive mesh in MM4. J Nanjing Inst. Meteor. (to be published, in Chinese)
[6]	Zhu Qiangen, Lin Jinrui, Shou Shouwen, et al., 1992. Principles and methods of synoptics (in Chinese). Beijing: China Meteorological Press. 715-781.