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1996年 8月上旬 ,8号台风倒槽移至河南省海河流域太行山东麓山丘区 ,自南向北形成了一条强降雨带 ,在安阳河、淇河、峪河、石门河等河上中游形成数个暴雨中心 ,这场暴雨强度大、历时短 ,大部分山丘区河道洪水暴涨 ,卫河干流主要水文测站测得洪水位大都超过保证水位 ,有的接近历史最高洪水位 ,部分河道漫堤决口 ,卫河各坡洼相继自然滞洪 ,这场洪水是海河流域 196 3年大洪水以后发生的又一场大洪水。分析了河南省海河流域“96· 8”暴雨洪水的情况及灾害的成因 ,提出了减轻洪水灾害应采取的对策措施
In early August 1996, No. 8 typhoon inverted trough moved to the hilly area of Taihang Mountain in Haihe River Basin, Henan Province, forming a strong rainfall zone from south to north and formed in the upper reaches of the river, such as Anyang River, Qihe River, Yuhe River and Shimen River Several heavy rainstorm centers, heavy rainfall intensity, lasted a short time, most of the hills and river floods, the major hydrological stations Weihe main hydrological stations measured over the guaranteed water level, and some close to the historical highest flood level, part of the river Dike Bukou, Wei River slope depression have natural detention floods, the flood is the Haihe River Basin after 196 floods occurred another big flood. Analyzed the situation of “96 · 8” storm flood and the cause of disaster in Haihe River Basin in Henan Province, and put forward the countermeasures to be taken to reduce flood disasters