3) glacier lake outburst
冰湖溃决
1.
Preliminary study on debris flow induced by glacier lake outburst in Tibet;
西藏典型冰湖溃决型泥石流的初步研究
2.
Progress in glacier lake outburst assessment system
冰湖溃决评价体系研究进展
5) glacial lakes outburst floods
冰湖溃决洪水
6) glacier debris flow
冰川泥石流
1.
The study area is located in Tibet along the Sichuan Tibet highway where 30 glacier debris flow gullies are selected for study.
选择流域面积、沟床比降、岩性系数、构造系数、冰川坡度、平均坡度、可移方量、最大淤积、冰川面积与流域面积的比值等因素作为冰川泥石流沟活动性评价的主要因素 ,应用因子分析方法确定了各因素的权重 ,并运用模糊关系理论建立了冰川泥石流活动性的评价方法。
2.
The Palongzangbu River basin in Tibet is a model area of glacier debris flow, and 59 debris flow valleys of different type are distributed along north bank of the main stream from Ranwu to Palong.
西藏帕隆藏布是典型的冰川泥石流区 ,其干流然乌至迫龙段右岸分布 5 9条各类泥石流沟。
3.
Research results show that the glacier debris flow along the Dushanzi-Korla Highway is insmall scale and has full process of development.
对独库公路冰川泥石流的考察及重点泥石流沟的观测，摸清了９条泥石流沟的分布，泥石流发生概况、危害和形成的水文气象条件。
补充资料：冰湖
1.结了冰的湖泊。 2.高山洼处冰川消失后形成的湖泊。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条