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Mapping of moraine dammed glacial lakes and assessment of their areal changes in the central and eastern Himalayas using satellite data 被引量:3
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作者 Sazeda BEGAM Dhrubajyoti SEN 《Journal of Mountain Science》 SCIE CSCD 2019年第1期77-94,共18页
The relatively rapid recession of glaciers in the Himalayas and formation of moraine dammed glacial lakes(MDGLs) in the recent past have increased the risk of glacier lake outburst floods(GLOF) in the countries of Nep... The relatively rapid recession of glaciers in the Himalayas and formation of moraine dammed glacial lakes(MDGLs) in the recent past have increased the risk of glacier lake outburst floods(GLOF) in the countries of Nepal and Bhutan and in the mountainous territory of Sikkim in India. As a product of climate change and global warming, such a risk has not only raised the level of threats to the habitation and infrastructure of the region, but has also contributed to the worsening of the balance of the unique ecosystem that exists in this domain that sustains several of the highest mountain peaks of the world. This study attempts to present an up to date mapping of the MDGLs in the central and eastern Himalayan regions using remote sensing data, with an objective to analyse their surface area variations with time from 1990 through 2015, disaggregated over six episodes. The study also includes the evaluation for susceptibility of MDGLs to GLOF with the least criteria decision analysis(LCDA). Forty two major MDGLs, each having a lake surface area greater than 0.2 km2, that were identified in the Himalayan ranges of Nepal, Bhutan, and Sikkim, have been categorized according to their surface area expansion rates in space and time. The lakes have been identified as located within the elevation range of 3800 m and6800 m above mean sea level(a msl). With a total surface area of 37.9 km2, these MDGLs as a whole were observed to have expanded by an astonishing 43.6% in area over the 25 year period of this study. A factor is introduced to numerically sort the lakes in terms of their relative yearly expansion rates, based on their interpretation of their surface area extents from satellite imageries. Verification of predicted GLOF events in the past using this factor with the limited field data as reported in literature indicates that the present analysis may be considered a sufficiently reliable and rapid technique for assessing the potential bursting susceptibility of the MDGLs. The analysis also indicates that, as of now, there are eight MDGLs in the region which appear to be in highly vulnerable states and have high chances in causing potential GLOF events anytime in the recent future. 展开更多
关键词 GLACIER RETREAT lakeS MAPPING moraine dammed glacial lake(mdgl) Surface area change of lakeS Landsat imagery data Least criteria decision analysis(LCDA)
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Moraine-dammed glacial lake changes during the recent 40 years in the Poiqu River Basin,Himalayas
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作者 XiuJuan Zhang ShiYin Liu Li Liu 《Research in Cold and Arid Regions》 CSCD 2015年第6期654-665,共12页
Glacier retreat is not only a symbol of temperature and precipitation change, but a dominating factor of glacial lake changes in alpine regions, which are of wide concern for high risk of potential outburst floods. Of... Glacier retreat is not only a symbol of temperature and precipitation change, but a dominating factor of glacial lake changes in alpine regions, which are of wide concern for high risk of potential outburst floods. Of all types of glacial lakes, moraine-dammed lakes may be the most dangerous to local residents in mountain regions. Thus, we monitored the dy- namics of 12 moraine-dammed glacial lakes from 1974 to 2014 in the Poiqu River Basin of central west Himalayas, as well as their associated glaciers with a combination of remote sensing, topographic maps and digital elevation models (DEMs). Our results indicate that all monitored moraine-dammed glacial lakes have expanded by 7.46 km2 in total while the glaciers retreated by a total of 15.29 km2 correspondingly. Meteorological analysis indicates a warming and drying trend in the Nyalam region from 1974 to 2014, which accelerated glacier retreat and then augmented the supply of moraine-dammed glacial lakes from glacier melt. Lake volume and water depth changed from 1974 to 2014 which indicates that lakes Kangxico, Galongco, and Youmojanco have a high potential for outburst floods and in urgent need for continuous moni- toring or artificial excavation to release water due to the quick increase in water depths and storage capacities. Lakes Jialongco and Cirenmaco, with outburst floods in 1981 and 2002, have a high potential risk for outburst floods because of rapid lake growth and steep slope gradients surrounding them. 展开更多
关键词 moraine-dammed glacial lake Poiqu River Basin remote sensing empirical equations slope gradient
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A framework of numerical simulation on moraine-dammed glacial lake outburst floods
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作者 ZHANG Xiujuan LIU Shiyin 《Journal of Arid Land》 SCIE CSCD 2015年第6期728-740,共13页
Glacial outburst floods(GLOFs) in alpine regions tend to be relatively complicated, multi-stage catastrophes, capable of causing significant geomorphologic changes in channel surroundings and posing severe threats t... Glacial outburst floods(GLOFs) in alpine regions tend to be relatively complicated, multi-stage catastrophes, capable of causing significant geomorphologic changes in channel surroundings and posing severe threats to infrastructure and the safety and livelihoods of human communities. GLOF disasters have been observed and potential hazards can be foreseen due to the newly formed glacial lakes or the expansion of existing ones in the Poiqu River Basin in Tibet, China. Here we presented a synthesis of GLOF-related studies including triggering mechanism(s), dam breach modeling, and flood routing simulation that have been employed to reconstruct or forecast GLOF hydrographs. We provided a framework for probability-based GLOFs simulation and hazard mapping in the Poiqu River Basin according to available knowledge. We also discussed the uncertainties and challenges in the model chains, which may form the basis for further research. 展开更多
关键词 moraine-dammed glacial lakes glacial outburst floods dam breaching mechanisms dam-breach models flood routing models
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国内外冰碛湖溃决研究进展 被引量:11
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作者 刘建康 周路旭 《探矿工程(岩土钻掘工程)》 2018年第8期44-50,共7页
末次冰期以来,气候变暖导致全球高山地区的冰川环境变化剧烈,冰碛湖稳定性降低导致溃决频率增加,成为中国、尼泊尔、俄罗斯、秘鲁等10多个国家和地区频繁发生的冰川灾害类型之一。冰碛湖溃决诱发形成的洪水和泥石流,由于规模巨大、成灾... 末次冰期以来,气候变暖导致全球高山地区的冰川环境变化剧烈,冰碛湖稳定性降低导致溃决频率增加,成为中国、尼泊尔、俄罗斯、秘鲁等10多个国家和地区频繁发生的冰川灾害类型之一。冰碛湖溃决诱发形成的洪水和泥石流,由于规模巨大、成灾速度快和波及范围广等特点,造成下游地区的基础设施和生命财产遭受惨重损失。本文通过对国内外冰碛湖溃决事件、溃决诱因、溃决模式和溃决洪水特征4个方面研究现状和发展现状的梳理和分析,总结经验和思路,从而为冰碛湖溃决研究和评价提供借鉴和参考。 展开更多
关键词 冰湖溃决 冰湖 冰碛湖 冰川灾害
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藏东南交通干线(林芝段)冰湖溃决危险性分析与评价 被引量:4
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作者 周路旭 刘建康 陈龙 《自然灾害学报》 CSCD 北大核心 2020年第3期162-172,共11页
藏东南地区河流纵横,湖泊密集,在高山极高山地区分布有大量冰湖,随着全球气候变暖的影响,冰湖溃决灾害已严重威胁人民生命财产安全以及川藏线的通行安全,因此,为冰湖的危险程度做出准确有效的评价至关重要,但是针对藏东南林芝段具体情况... 藏东南地区河流纵横,湖泊密集,在高山极高山地区分布有大量冰湖,随着全球气候变暖的影响,冰湖溃决灾害已严重威胁人民生命财产安全以及川藏线的通行安全,因此,为冰湖的危险程度做出准确有效的评价至关重要,但是针对藏东南林芝段具体情况,传统的冰湖危险程度评价方法不够准确高效,本文在传统的评价方法基础之上应用Fisher判别分析方法,对研究区472个冰湖进行了判识,并作出危险性评价与分析,其中,评定出处于高度危险的冰湖有6个,危险程度为中的冰湖有10个,456冰湖危险程度均为低,分析GL09所在地区及其下游为高度危险区,多依隆巴、曲都隆巴、那琼隆巴、曲格隆巴及其下游为较危险区,其余冰湖危险程度为中的地区为相对安全地区,危险程度低的地区为安全地区,为全面评价与分析藏东南交通干线(林芝段)冰湖危险性,川藏铁路建设选址等方面提供了重要的参考价值。 展开更多
关键词 帕隆藏布 冰湖溃决 冰碛湖 危险性评价 藏东南
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冰滑坡涌浪下冰碛坝溃决机理试验研究 被引量:2
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作者 李慧斌 陈华勇 +2 位作者 Robin Neupane 阮合春 李霄 《水土保持通报》 CSCD 北大核心 2021年第2期25-34,42,共11页
[目的]对冰滑坡涌浪导致的冰碛坝溃决过程与溃决机理进行试验研究,为冰川区重大工程建设和冰湖冰碛坝溃决灾害防治提供科技支撑。[方法]开展不同滑块体积、滑动角度、滑动距离、坝体物质组成和坝体几何形态的水槽模型试验。基于试验现... [目的]对冰滑坡涌浪导致的冰碛坝溃决过程与溃决机理进行试验研究,为冰川区重大工程建设和冰湖冰碛坝溃决灾害防治提供科技支撑。[方法]开展不同滑块体积、滑动角度、滑动距离、坝体物质组成和坝体几何形态的水槽模型试验。基于试验现象、试验数据与理论推导,对涌浪过程、坝体物质起动和坝体溃决临界条件进行分析。[结果]①冰滑坡涌浪随时间和距离不断衰减,其随时间衰减显著。②将涌浪作用下的溃决过程分为坡面侵蚀、陡坎侵蚀、侧向侵蚀和衰退4个阶段,其中侧向侵蚀阶段的溃决流量最大,流速最快,侵蚀能力最强。③从颗粒起动机理的角度给出了颗粒起动流速,与沙莫夫公式进行对比分析,对比结果较为吻合。④基于能量守恒原理得到了冰湖溃决事件发生的临界条件,通过西藏自治区林芝市波密县米堆沟光谢错冰湖溃决事件进行验证,验证结果良好。[结论]冰湖库容越大、坝前水深越深、涌浪高度越高,坝体越易发生溃决;冰碛坝堆积物中细颗粒含量越高,坝体颗粒间黏附力越强,坝体越稳定;冰碛坝坝宽及下游坡脚越大,坝体越稳定,溃决所需时间越长。 展开更多
关键词 冰湖溃决 冰滑坡涌浪 冰碛坝 洪峰流量 起动机理 溃决临界条件
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西藏喜马拉雅山区危险冰湖及其溃决特征 被引量:83
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作者 徐道明 冯清华 《地理学报》 EI CSSCI CSCD 北大核心 1989年第3期343-352,共10页
喜马拉雅山区的冰湖溃决主要属终碛湖溃决。野外考察和编目研究的结果表明,终碛湖占各类高山冰湖总数的1/2和总水体的3/4。鉴别出34个危险终碛湖,其水体容量在10×10~6—30×10~6m^3之间,平均水深31m,实测最大水深在70m左... 喜马拉雅山区的冰湖溃决主要属终碛湖溃决。野外考察和编目研究的结果表明,终碛湖占各类高山冰湖总数的1/2和总水体的3/4。鉴别出34个危险终碛湖,其水体容量在10×10~6—30×10~6m^3之间,平均水深31m,实测最大水深在70m左右。危险终碛湖绝大多数形成于小冰期最后一次冰退阶段,由于其形态特征和现代冰川的直接影响而具有潜在的溃决危险;讨论了终碛湖溃决的特征,主要因素及其周期性。 展开更多
关键词 冰湖 溃决 喜马拉雅山区
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冰崩涌浪作用下的冰湖溃决过程试验研究
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作者 阮合春 陈华勇 +4 位作者 陈晓清 赵万玉 陈剑刚 李霄 俞昀晗 《科学技术与工程》 北大核心 2023年第29期12391-12398,共8页
冰崩涌浪是导致冰湖溃决的一个主要的诱发因素之一。通过水槽模型试验,研究了在冰崩涌浪作用下,不同坝体颗粒级配、坝高、下游坝坡坡度对冰碛坝溃决过程的影响,揭示了涌浪对溃决过程的影响机制,并得到了冰碛坝溃决的临界条件。结果表明... 冰崩涌浪是导致冰湖溃决的一个主要的诱发因素之一。通过水槽模型试验,研究了在冰崩涌浪作用下,不同坝体颗粒级配、坝高、下游坝坡坡度对冰碛坝溃决过程的影响,揭示了涌浪对溃决过程的影响机制,并得到了冰碛坝溃决的临界条件。结果表明:冰碛坝存在漫顶溃决、坝坡失稳、管涌破坏3种溃决模式;根据冰崩涌浪对坝体的侵蚀效应,结合溃口的纵向演化过程,将冰碛坝的溃决过程划分为涌浪侵蚀阶段(阶段Ⅰ)、库区小扰动溢流侵蚀阶段(阶段Ⅱ);涌浪过坝后的强水动力条件增加了坝体的侵蚀率,当溃口贯通后,涌浪已基本消散,溃决过程转为正常的溢流溃决,并且涌浪向坝体提供了高频瞬时荷载,削减了坝体稳定性;从动力学的角度提出了冰碛坝临界溃决条件的判定方法;冰湖溃决洪峰流量与坝高和下游坝坡呈现正相关,与坝体中值粒径D_(50)呈现负相关关系。 展开更多
关键词 冰崩涌浪 冰湖溃决 冰碛坝 洪峰流量 溃决过程
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20世纪以来西藏冰湖溃决灾害事件梳理 被引量:61
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作者 姚晓军 刘时银 +1 位作者 孙美平 张秀娟 《自然资源学报》 CSSCI CSCD 北大核心 2014年第8期1377-1390,共14页
冰湖溃决洪水(泥石流)是西藏自治区主要自然灾害之一,对已溃决冰湖特征及灾害影响范围与程度的认识是判定冰湖溃决条件、构建冰湖溃决评价指标体系以及开展冰湖溃决洪水估算与模拟的基础。通过对已溃决冰湖灾害事件文献及资料整理,结合... 冰湖溃决洪水(泥石流)是西藏自治区主要自然灾害之一,对已溃决冰湖特征及灾害影响范围与程度的认识是判定冰湖溃决条件、构建冰湖溃决评价指标体系以及开展冰湖溃决洪水估算与模拟的基础。通过对已溃决冰湖灾害事件文献及资料整理,结合地形图、遥感影像、中国冰川编目数据、Google Earth、冰湖溃决遗迹记录及野外考察,系统梳理了20世纪以来西藏地区发生的27次冰湖溃决事件,从多个角度判定并给出了23个已溃决冰湖所在的地理位置,并对金错、印达普错和次拉错冰湖溃决事件描述进行了勘误,指出1982年8月27日在定结县发生的冰湖灾害事件应是印达普错溃决所导致,2009年7月29日在边坝县发生溃决的冰湖是错嘎,而非次拉错。 展开更多
关键词 冰湖溃决洪水 泥石流 冰碛湖 西藏
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