1) ice jam flood
凌汛特点
2) ice run
凌汛
3) Ice flood
凌汛
1.
Application of CBERS-02 on ice flood monitoring of Yellow River;
中巴地球资源一号02星在黄河凌汛监测中的应用
2.
During 1950~1967 years before commissioning of Liujiaxia reservoir, there took place ice floods resulting in eight breaches of dikes in the Ningxia-Inner Mongolia reach of Yellow River.
黄河宁蒙河段,在刘家峡水库投运前的1950～1967年间,宁蒙河段凌汛灾害引起堤防决口8次。
3.
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。
4) ice jam flood
凌汛
1.
Ice jam disaster has been often happened in the Chinese history, particularly in the period of last 100 years after the Tongwaxiang break and change courses of the Yellow River in 1855 till 1955, ice jam floods occurred in 29 years and nearly 100 breaks took place with a frequency of once in 3.
历史上黄河凌汛灾害严重,特别是清咸丰五年(1855年)铜瓦厢决口改道后至1955年的100年中,发生凌汛决溢的年份达29年,决口近百处,平均三年半就有1年发生凌汛灾害。
2.
The lower reaches of the Yellow River is an instability frozen cover section, and ice jam conditions complex , and ice jam flooding occurred frequency in history.
但由于凌汛的发生带有很大的突发性,冰塞、冰坝难以预测,加之河道持续淤积萎缩,弯道和浮桥众多,影响凌汛的热力因素无法控制等,黄河下游防凌仍将是长期任务,今后防凌工作还有许多问题需重点研究。
5) cause of ice flood
凌汛成因
6) the ice flood season
凌汛期
1.
Analysis of river water flow evolution in the ice flood season in the downstream of Yellow River;
黄河下游凌汛期河道水流演进计算分析
参考词条
补充资料：冰凌洪水(见凌汛)
冰凌洪水(见凌汛)
bingling hongshu-冰凌洪水见凌汛。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。