Abstract:The main mountain range of Jiuhua mountain and the surrounding terrain cover an area from Tiantai to Dahuatai, which is surrounded by low hills. In such a complex terrain, the climate difference is obvious. Applying observational data (1980-2010), including automatic weather station at different altitudes and using theory of atmospheric boundary layer and mathematical statistics, cloud water differences between the mountains and hills have been investigated. The results show that the dynamic factor of the terrain has changed the vapor transport conditions of the mountain; the mountains have a more obvious effect on rainfall, and the greater the precipitation intensity is, the more obvious role it plays; the average contribution rate of the terrain precipitation is 37.6%. Mountains and the surrounding's precipitation distribution is very uneven, and Jiuhuashan's average annual rainfall is 34.1% more than the surrounding area's. Water resource in mountain is much larger than in the surrounding hilly areas, the former is 3.4 times more than that of the latter, and there is a surplus all the year, but the distribution is uneven. Autumn is the driest season. It is necessary to find out open source water storage and to be added by artificial rainfall to alleviate the drought of the mountains.