摘要
2013年"菲特"台风影响期间,上海地区普降大暴雨。在降雨、风暴潮增水和上游来水的共同影响下,黄浦江、长江口、杭州湾潮位全线超警,特别是黄浦江上游部分测站最高潮位超历史记录,严重制约了流域排洪和区域排涝。为分析台风影响期间太湖流域上游来水对上海地区的影响,通过现场调查、统计分析和模型模拟等方法,计算分析台风影响期间太湖流域产水量、外边界进出水量、湖库河网调蓄量以及洪涝灾害严重地区的淹涝量等,从而计算太湖流域上游进入上海地区的水量,为上海地区的防洪减灾工作提供基础支撑。
During Typhoon Fitow in 2013, the storm rain occurred in Shanghai area. Under the affect of the rainfall, storm surge and inflow from the upper reaches, the water level and tide level all exceeded the warning stages in the Huangpujiang River,Yangtze River Estuary and Hangzhou Bay. Especially, some levels even got over the historical records at the some stations in the upper reaches of the Huangpu River. In order to study the effect of the inflow from the upper reaches of the Taihu Basin on Shanghai area during the Typhoon, the paper analyzed the water production, inflow and outflow of the outer boundary, storage capacity of the lakes and reservoirs, and submergence quantity during the Typhoon by investigation, scientific statistics and model calculation. And then it made calculation of the inflow into Shanghai area to provide basic support for flood control and disaster mitigation in Shanghai.
出处
《水文》
CSCD
北大核心
2014年第6期93-95,共3页
Journal of China Hydrology
