首页|藏东南乌连沟石冰川活动特征与灾变机制

藏东南乌连沟石冰川活动特征与灾变机制

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全球气候变暖背景下,青藏高原的石冰川活动性增强,产生灾变的趋势上升。采用遥感影像分析、现场调查及气象和径流监测等方法,获取了藏东南地区乌连沟石冰川的特征数据,分析其灾变形成泥石流的诱发因素及过程。结果显示,乌连沟石冰川2010-2017年平均运动速度为1~3 m·a-1,且前缘整体运动速度显著高于中后部。石冰川前缘向前运动进而失稳,可持续为沟道输送松散物源,2013年及2014年约有5 600~9 000 m3石冰川输送的松散物质被启动。形成泥石流除需要充沛的物源外,还需要足够的水源启动。区内降雨量有限,乌连沟最大径流出现在5-6月,主要由高温引发冰雪消融贡献。分析2013年及2014年两次泥石流事件发现,其主要诱发因素是高温,灾变机制为气温快速升高导致表层冰雪快速消融,融水在石冰川表面凹陷处积聚形成湖塘,湖水泄流启动了石冰川前缘积累的松散物质形成泥石流。未来随着气候变暖加剧,石冰川的活动性进一步增强,在急剧升温或强降雨影响下,形成泥石流的规模及频率可能会增加,需防范石冰川灾变形成泥石流的致灾风险。
Activity and catastrophe mechanism of the rock glacier in the Wulian Gully,southeast Qinghai-Xizang Plateau
Against the backdrop of global climate warming,the activity of rock glaciers in the Qinghai-Xizang Plateau has been enhanced,leading to an increasing trend of disasters.By using methods such as remote sensing image analysis,field investigation,meteorological and runoff monitoring,characteristic data of the Wulian rock glacier in southeastern Qinghai-Xizang Plateau were obtained,and the triggering factors and processes of the for-mation of debris flows were analyzed.The findings indicate that the Wulian rock glacier's mean velocity ranged from 1~3 m·a-1 between 2010 and 2017,with the frontal velocity being substantially higher than that of the mid-dle and rear.This advancement and associated instability of the rock glacier front can be attributed to the channel transportation of loose material sources.Notably,the rock glacier transported approximately 5 600~9 000 m3 of loose material,which triggered debris flow events in 2013 and 2014.The generation of such flows requires not only abundant loose sources but also sufficient water to initiate.In this study,the maximum runoff occurred dur-ing May and June,primarily driven by the melting of ice and snow resulting from elevated temperatures.By ex-amining the two debris flow events,it was discovered that high temperature was the primary contributing factor,and the disaster mechanism involved the rapid melting of surface ice and snow due to elevated temperatures,causing the accumulation of meltwater in depressions on the rock glacier surface,resulting in a pond that,when discharged,caused loose material in front of the rock Glacier to form debris flow.As climate warming exacer-bates in the future,rock glacier activity is anticipated to increase.Additionally,under the influence of rapid warming or heavy rainfall,the scale and frequency of debris flows may increase.Therefore,it is imperative to mitigate the risk of rock glacier disaster formation through debris flow prevention measures.

rock glacierdebris flowQinghai-Xizang Plateauclimate change

李元灵、余斌、黄海、陈龙、杨东旭、张佳佳、高波、田尤、李洪梁、罗伦

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成都理工大学 环境与土木工程学院,四川 成都 610059

中国地质科学院 探矿工艺研究所,四川 成都 611734

自然资源部地质灾害风险防控工程技术创新中心,四川 成都 611734

中国科学院 青藏高原研究所,北京 100101

中国地质调查局 军民融合地质调查中心,四川 成都 610036

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石冰川 泥石流 青藏高原 气候变化

中国地质调查局项目中国地质调查局项目第二次青藏高原综合科学考察研究项目国家自然科学基金项目

DD20190644DD202217412019QZKK090241807300

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(2)
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