The Langmoche Flashflood, Khumbu Himal, Nepal
The Langmoche Flashflood, Khumbu Himal, Nepal
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DOI：
10.2307/3673345
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发表时间：
1986-02
影响因子：
1.6
通讯作者：
D. Vuichard;Markus N. Zimmermann
中科院分区：
文献类型：
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作者：
D. Vuichard;Markus N. Zimmermann
1985年8月4日，尼泊尔东部昆布地区纳姆切巴扎尔上方的一个冰川湖爆发。在严重冰川化的山区，必须预料到这种山洪暴发。它们有几种：（1）被冰川阻塞的湖泊的灾难性爆发，或者来自冰川系统之下或内部的融水的积水的爆发;（2）被旧的末端冰碛阻塞的冰川前面的湖泊的溢出;（3）被山体滑坡、落石或雪或冰雪崩阻塞的短暂湖泊的突然排水，这些湖泊阻塞了河流的主要通道。的结果
On 4 August 1985 an outburst of a glacial lake occurred in the Khumbu area of eastern Nepal above Namche Bazar. Such flash-floods must be anticipated in heavily glacierized mountain regions. They are of several kinds: (1) the catastrophic outbreak of lakes dammed by a glacier, or the outbreak of ponded melt-water from beneath or within a glacier system; (2) the overspill of lakes frontal to a glacier that have been dammed by old end moraines; and (3) the sudden drainage of ephemeral lakes dammed by landslides, rockfalls, or by snow or ice avalanches, that have blocked the main channel of a river. The results of