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2篇 您的检索式:作者名="Liang Biqi"
    题名 作者 年代 出处 被引量
1THE TYPHOON DISASTERS AND RELATED EFFECTS IN CHINA显示文摘China is one of the countries which were affected very seriously by tropical cyclones. In this paper, the active features of tropical cyclones which affected and landfell over China, the distinguishing characteristics of typhoon disasters and related formation laws have been studied, and the impact of trphoon disasters on China’s socio-economic development have been discussed. The study reveals that typhoon disasters which affected China are characterized by high freqency in occurrence, violent in sudden occurrence, remarkable effects in China,widescope in impact and severe intensities in disasters, and this type of disaster was caused by huge gales, rainstorms, storm surges and reatal chain-disasters.Typhoon disasters have not only caused great casualties but also exerted severe effects on every economic departments in China. There is an annual increasing tendency in direct economic loss caused by taphoon disasters and since 1990, the annual average economic loss has totalled up to over lo billion RMB yuan.Liang Biqi Wen Zhiqing Liang Jingqing (Department of Atmospheric Science, Zhongshan University, Guanghou 510275People’s Republic of China) 1996Journal of Geographical Sciences1996,6,1:7
2A comparison analysis between developed and undeveloped depressions over the South China Sea显示文摘- In this paper, by using two sets of composite data of developed and undeveloped depressions over the South China Sea, we analyze and compare the dynamic structures, the heating fields and the vorticity budget residuals of two different types of depressions. Our conclusions are as follows:The two types of depressions are similar in thermodynamical and dynamical structures. The main differ ences are : in the high layer of developed depression there is a divergence field, with a center near the zero line of vertical wind shear, and over undeveloped depression, the divergence field is weaker and the vertical wind at its center is greater than 5 m s-1. The thermodynamical field of the former is asymmetrical and that of the latter is quasi - symmetrical. As far as the dynamics structure is concerned, the convergence in the lower layer and the difference of divergence between the upper and lower layers of developed depression is three tmies larger than that of undeveloped depression. The upward motion andLiang Biqi Zhang Qiuqing Department of Atmospheric Sciences, Zhongshan University, Guangzhou, China National Research Center for Marine Environment Forcasts, Beijing, China 1989Acta Oceanologica Sinica1989,8,2:0
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