Digital Terrain Modelling Using Corona and ALOS PRISM Data to Investigate the Distal Part of Imja Glacier,Khumbu Himal,Nepal
Digital Terrain Modelling Using Corona and ALOS PRISM Data to Investigate the Distal Part of Imja Glacier,Khumbu Himal,Nepal作者机构:Graduate School of Environmental ScienceHokkaido University Faculty of Environmental Earth ScienceHokkaido University
出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))
年 卷 期:2011年第8卷第3期
页 面:390-402页
核心收录:
学科分类:07[理学] 0705[理学-地理学] 070501[理学-自然地理学]
基 金:the Japan Science Society (Sasagawa Research Fund) the Global Centre of Excellence (GCOE) programme by JSPS for partial funding
主 题:Imja Glacier Nepal Himalaya DTM Topographic map Surface lowering Corona ALOS PRISM
摘 要:This study used Corona KH-4A and Advanced Land Observing Satellite (ALOS) PRISM images to generate digital terrain models (DTMs) of the distal part of Imja Glacier,where a few supraglacial ponds (~0.07 km 2) expanded into the large Imja Glacier Lake (Imja Tsho,~0.91 km 2) between 1964 and *** and subsequently derived topographical maps with contour intervals of 1 m were created from the high-resolution images (Corona in 1964 and ALOS in 2006) in the Leica Photogrammetric Suite (LPS) *** DTMs and topographic maps provided excellent representation of the elevation and micro-topography of the glacier surface,such as its supra-glacial ponds/lake,surface depressions,and moraine ridges,with an error of about +/-4 m (maximum).The DTMs produced from the Corona and ALOS PRISM images are suitable for use in studies of the surface change of *** topographical maps produced from the Corona data (1964) showed that part of the dead ice in the down-glacier area was even higher than the top of the lateral moraine ridges,while the glacier surface in the up-glacier area was noticeably lower than the moraine *** suggests more extensive melting of glacier ice in the up-glacier area before *** average lowering of the glacier surface from 1964 to 2006 was 16.9 m for the dead-ice area west of the lake and 47.4 m for the glacier surface east of the lake;between 1964 and 2002,the lake surface lowered by 82.3 *** figures represent average lowering rates of 0.4,1.1,and 2.2 m/year for the respective areas.