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汉语拼音：líng xùn

由于上游冰雪融化，下游河道尚未解冻而出现的河水暴涨现象。

1. 上游冰雪融化，而下游尚未解冻所形成的河水猛涨。

   清 陈康祺 《郎潜纪闻》卷十：“ 黄河 水信……冬曰凌汛，十月曰伏槽水，十一月十二月曰蹙凌水。”

• The ice flood is one of the serious natural disasters in the lower reaches of Yellow River.

  凌汛是黄河下游严重的自然灾害之一，黄河下游天桥河段属于典型的弯曲窄河段，极易发生凌情。

• People's Yellow River has made the 52-year-volt burst of autumn Tai Xun is not a great victory, and defeat a number of serious ice run.

  取得了人民治理黄河52年伏秋大汛不决口的伟大胜利，并战胜多次严重凌汛。

• This paper analyzed the ice slush formation mechanism, change process and ice flood cause of the Yellow River in Inner Mongolia.

  本文着重分析研究黄河内蒙古段冰凌形成机理、冰情演变及凌汛成因。

• And this has an important practical significance on avoiding the occurrence of disasters, reducing the threat of ice flood.

  冰盖下的水流结构的研究，在避免灾害的发生、减轻凌汛威胁方面，有着重要的现实意义。

• Year Dongmochunchu, Inner Mongolia, Shandong, river and downstream sections of ice flood disasters have occurred.

  每年冬末春初，内蒙古河段和下游山东河段，凌汛灾害时有发生。

• Sedimentation Shrivel in Ningxia-Inner Mongolia Section of the Yellow River and Its Influence to Ice Run Floods

  黄河宁蒙河段河道淤积萎缩及其对凌汛的影响

• Characteristics and Causes of Ice Flood in Ningxia-Inner Mongolia Section of the Yellow River Valley

  黄河宁蒙河段凌汛特征及成因分析

• The cause analysis and countermeasures of ice flood disaster in main stream from Yumenkou to Tongguan reach of Yellow river

  黄河小北干流河段凌汛灾害成因分析及其对策

• Application of non-linear combination forecast method of system to ice flood prediction of the Yellow River

  系统非线性组合预测方法及在黄河凌汛预测中应用