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本文分析了造成黄河“96·8”洪水的气象成因：西风带有弱冷空气东移南下，影响三门峡至花园口区间；西太平洋副热带高压势力较强，脊线偏北，西伸显著，并且在三门峡—花园口区间东北部形成一个西北—东南向的高压脊，使三门峡至花园口区间成为水汽输入、能量聚集的区域，极有利于暴雨的产生和维持；减弱的台风倒槽和东南风急流影响三门峡至花园口区间，造成大量水汽输入、强烈辐合上升运动，为暴雨提供了有利的水汽、动力条件。另外，三门峡至花园口区间的特殊地形对暴雨的加强和持续有一定作用。
This paper analyzes the meteorological causes of the “96 · 8” flood in the Yellow River: the westerly winds with weak cold air moving eastward and southward affect the Sanmenxia-Huayuankou interval; the western Pacific subtropical high has strong forces, the ridge lines are northward and the westward extensibility is significant, and The formation of a northwest-southeast high ridge in the northeast of Sanmenxia-Huayuankou interval made the Sanmenxia-Huayuankou interval an area with water vapor input and energy accumulation, which is very conducive to the occurrence and maintenance of heavy rain. Weakened typhoon trough and southeast jet stream Affecting Sanmenxia to Huayuankou interval, resulting in a large amount of water vapor input, strong convergence rising movement, providing favorable conditions for the rainstorm, water vapor. In addition, Sanmenxia to Huayuankou special terrain on the strengthening and continued heavy rain have a certain effect.