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Himalayan glaciers: combining remote sensing, field techniques and indigenous knowledge to understand spatio-temporal patterns of glacier changes and their impact on water resources

机译:喜马拉雅冰川:结合遥感,野外技术和本土知识,了解冰川变化的时空格局及其对水资源的影响

摘要

With contradictory statements about u22disappearing Himalayan glaciersu22 in the last few years, increasing concerns have been raised about the impact of snow and glacier changes on regional water supplies. Concomitantly, local communities in the western Himalaya report changes in glacier extents, snow cover and weather patterns. In response to perceived water scarcity, indigenous Himalayan cultures have begun a number of adaptive responses such as meltwater harvesting to construct u22artificialu22 glaciers. This research addresses the need for a detailed assessment of glacier and climate parameters in the Himalaya, with the goal of identifying u22at risku22 glacierized areas and helping these local communities plan future water resources. The objectives of the research are threefold: 1) to review existing knowledge about glacier fluctuations and remote sensing methods for glacier mapping in the Himalaya; 3) to quantify spatio-temporal patterns of glacier changes in the eastern Himalaya in the last decades using remote sensing techniques and field measurements and 3) to quantify the role of glacier melt to streamflow using a combination of remote sensing and isotopic techniques. This thesis focuses on the monsoon-influenced eastern Himalaya (the Langtang and Khumbu regions in the Nepal Himalaya, and Sikkim in the Indian Himalaya). The research is grounded in extensive field surveys conducted from 2006 to 2010 across the Himalaya, including glacier mass balance expeditions, water sampling, ground-control point (GCP) acquisition and GPS-enabled photos. The goal of this research is to understand how topographic and climatic factors influence the rates of glacier change at various spatial scales, and how these changes re likely to affect future water resources. Multi-temporal (decadal) glacier datasets were derived from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) sensor, Landsat ETM+, older topographic maps, declassified Corona imagery and very high-resolution QuickBird and Ikonos imagery. I used a combination of visible, near infrared and thermal multispectral data combined with texture analysis and topography for glacier mapping. The results of this research help fill a gap in the understanding of glacier patterns in the data-scarce eastern Himalaya. The results of this research are useful for assessing vulnerability of the Himalaya to water scarcity due to future glacier or climate changes.
机译:在过去的几年中,关于 u22喜马拉雅冰川消失的矛盾说法,人们越来越关注降雪和冰川变化对区域供水的影响。随之而来的是,喜马拉雅西部的当地社区报告了冰川范围,积雪和天气模式的变化。为了应对人们认为的水资源短缺,喜马拉雅土著文化已开始采取许多适应性措施,例如收集融水来建造“人造”冰川。这项研究满足了对喜马拉雅山冰川和气候参数进行详细评估的需求,目的是确定处于冰川风险的地区并帮助这些当地社区规划未来的水资源。研究的目的有三方面:1)回顾关于喜马拉雅山冰川变化和冰川映射遥感方法的现有知识; 3)使用遥感技术和野外测量来量化喜马拉雅东部近几十年来冰川变化的时空格局; 3)使用遥感和同位素技术相结合的方法来量化冰川融化在河流中的作用。本文主要研究季风影响的东部喜马拉雅山脉(尼泊尔喜马拉雅山脉的朗唐和昆布地区,以及印度喜马拉雅山脉的锡金地区)。该研究的基础是2006年至2010年在喜马拉雅地区进行的广泛野外调查,其中包括冰川质量平衡探险,水采样,地面控制点(GCP)采集和GPS启用的照片。这项研究的目的是了解地形和气候因素如何影响各种空间尺度上的冰川变化速率,以及这些变化如何可能影响未来的水资源。多时相(年代际)冰川数据集来自高级星载热发射和反射辐射计(ASTER)传感器,Landsat ETM +,较旧的地形图,解密的电晕图像以及超高分辨率的QuickBird和Ikonos图像。我将可见,近红外和热多光谱数据与纹理分析和地形相结合,用于冰川测绘。这项研究的结果有助于填补对缺乏数据的东部喜马拉雅山冰川模式的了解的空白。这项研究的结果可用于评估喜马拉雅山因未来冰川或气候变化而对水资源短缺的脆弱性。

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    Racoviteanu Adina;

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  • 年度 2011
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