摘要
2010年6月16~24日,洞庭湖和鄱阳湖水系发生强降雨,两湖水系主要江河均发生超警洪水,鄱阳湖水系抚河、信江洪峰水位接近历史最高。为了解该次强降雨过程,详细分析了两湖水系的降雨实况和造成强降雨的天气成因,并对该次强降雨过程期间所开展的降雨预报与实况进行了检验,认为,采用天气学综合降雨预报方法对该次强降雨过程的预报较为成功,对该次暴雨过程的分析和预报实践可为今后提供宝贵经验和参考。
On June 16~24,2010,heavy rainstorm occurred in Poyang Lake and Dongting Lake areas in China,the level of the main rivers in these areas all reached warning water level,and especially,the flood peaks of Fuhe River and Xinjiang River in Poyang Lake system nearly reached the historically highest level.We present the precipitation condition and analyze the causes of the weather that induced the rainfall,and the heavy rainfall process and its meteorological comprehensive rainfall forecasting were checked by the practical rainfall process,so we conclude that the flood in the two lake areas was caused by the continuous heavy rainfall.
出处
《人民长江》
北大核心
2011年第6期32-34,共3页
Yangtze River
关键词
两湖水系
环流形势
强降雨条件
降雨检验
Poyang Lake and Dongting Lake system
atmospheric circulation pattern
condition of heavy rainfall
rainfall check