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引用本文:陆鸿宾,魏桂玲.太湖的降水效应.湖泊科学,1990,2(2):9-16. DOI:10.18307/1990.0202
Lu Hongbin,Wei Guiling.Precipitation Effect Of Taihu Lake. J. Lake Sci.1990,2(2):9-16. DOI:10.18307/1990.0202
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太湖的降水效应
陆鸿宾, 魏桂玲
中国科学院南京地理与湖泊研究所
摘要:
本文分析了太湖湖区降水的时空分布特征;估算和讨论了太湖的降水效应;揭示了太湖的降水效应不太显著;太湖湖区降水量的变化是该湖水位变化的决定性因素之一。
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DOI:10.18307/1990.0202
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Precipitation Effect Of Taihu Lake
Lu Hongbin, Wei Guiling
Nanjing Institute of Geography & Limnology, Acadcmia Sinica
Abstract:
The average annual precipitation of Taihu Lake is 950-1000mm on NE shores, which increases to 1200-1250mm on SW shores progressively. The annual precipitation course is characterized by a double-peak model with the maximum value being 147-105mm at all stations in Jun. and the minimum value 33-l8mm on the most stations in Dec.. The estimated precipitation effect of Taihu Lake shows that there exists a low value region of precipitation on the lake surface fundamentally. The precipitation effect of Taihu Lake enables the precipitation on lake shores to average 20mm less than that of far from the lake shores, <3% of the annual precipitation. This means that the influence of Taihu Lake on the precipitation is not evident, but it has a little impact on the precipitation distribution of this region. The precipitation on the Taihu Lake region is one of the decisive factors of the water level fluctuation.
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