气候变化研究进展2011，Vol.7Issue(6)：412-417,6.
气候变化影响下林芝地区泥石流发育规律研究
Development Rules of Debris Flow Under the Influence of Climate Change in Nyingchi
摘要
Abstract
Based on the typical debris flows in Nyingchi, this paper presents the basic type, distribution and movement of debris flows, analyzes the initiation condition and critical threshold, and discloses the incubation law of debris flows, and also the impact of temperature and rainfall changes on debris flow initiation. Glaciers debris flow may be inspired during temperature or rainfall increasing. If daily precipitation < 5 mm, melting ice and snow debris is stimulated mainly by temperature; when daily precipitation is 5-10 mm, mainly the glaciers-rainfall debris flow occurs; when daily precipitation >10 mm, rainfall debris flow is in dominate. Glacier debris flows under temperature increasing and decreasing account for 80% and 20%, respectively, while the rainfall debris flows account for 60% and 40%, repectively. Much rainfall are benefit for the initiation of debris flows.关键词
泥石流/气候变化/林芝地区Key words
debris flow/ climate change/ Nyingchi region分类
天文与地球科学引用本文复制引用
陈宁生,周海波,胡桂胜..气候变化影响下林芝地区泥石流发育规律研究[J].气候变化研究进展,2011,7(6):412-417,6.基金项目
国家科技支撑计划(2008BAB42B06) （2008BAB42B06）
