喀喇昆仑山厦呈、吕莫慕士塔格山段现代冰川分布及变化特征

doi:10.19388/j.zgdzdc.2017.03.07

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Abstract In the background of global warming and glaciers shrinking, the authors took the medium spatial resolution satellite data (ETM, Landsat 8) as the main data of remote sensing, and completed the remote sensing investigation of glaciers variation in Siachen and LyuMo Muztaghata Mountains by human-computer interactive interpretation, in order to reveal distribution and variation characteristics of the modern glaciers in Karakoram Mountain Range where mountain glaciers are well developed. The glaciers area, distribution and variation characteristics of a part of glaciers were ascertained in the study area. This study totally investigated 1 373 glaciers, including 554 glaciers in our country and 819 glaciers in India-controlled Kashmir. Also the ETM data and Landsat 8 data about the typical glaciers in the study area were contrasted. The result shows that the ice tongue shrinking, expanding and steadying exist at the same time, which can provide references for the study of glaciers variations in Karakoram Mountain Range. The results above have important scientific significance and practical value for the water resources utilization of our western frontier and prevention of snow disaster.

Key words： Karakoram Mountain Range ETM Landsat 8 remote sensing glacier

Received: 08 March 2017

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http://114.242.223.217/EN/10.19388/j.zgdzdc.2017.03.07 OR http://114.242.223.217/EN/Y2017/V4/I3/46

[1] 苏珍,谢自楚,王志超,等.喀喇昆仑山—昆仑山地区冰川与环境[M].北京:科学出版社,1998:33-35.
[2] 方洪宾,赵福岳,张振德,等.青藏高原现代生态地质环境遥感调查与演变研究[M].北京:地质出版社,2009:49.
[3] 张祥松,米德生.喀喇昆仑山现代冰川的研究[J].冰川冻土,1982,4(3):15-28.
[4] 陈亚宁,王志超.喀喇昆仑山北坡冰川地质及地貌[J].新疆地质,1991,9(3):284-290.
[5] 张瑞江.青藏高原冰川演变与生态地质环境响应[J].中国地质调查,2016,3(2):46-50.
[6] 聂洪峰,方洪宾,杨金中,等.国土遥感综合调查工程总体目标的设计与实现[J].中国地质调查,2016,3(5):1-6.
[7] 刘潮海,施雅风,王宗太,等.中国冰川资源及其分布特征——中国冰川目录编制完成[J].冰川冻土,2000,22(2):106-112.
[8] 刘时银,姚晓军,郭万钦,等.基于第二次冰川编目的中国冰川现状[J].地理学报,2015,70(1):3-16.
[9] Hewitt K.The Karakoram anomaly? Glacier expansion and the elevation effect,Karakoram Himalaya[J].Mount Res Dev,2005,25(4):332-340.
[10] Hewitt K.Tributary glacier surges:An exceptional concentration at Panmah Glacier,Karakoram Himalaya[J].J Glaciol,2007,53(181):181-188.
[11] Iturrizaga L.Historical and recent glacier variations in the Karakoram Mountains[J].Geophys Res Abst,2007(9):05470.
[12] 蒲健辰,姚檀栋,王宁练,等.近百年来青藏高原冰川的进退变化[J].冰川冻土,2004,26(5):517-522.
[13] 上官冬辉,刘时银,丁永建,等.中国喀喇昆仑山、慕士塔格公格尔山典型冰川变化监测结果[J].冰川冻土,2004,26(3):374-375.
[14] 施雅风,刘时银,上官冬辉,等.近30 a青藏高原气候与冰川变化中的两种特殊现象[J].气候变化研究进展,2006,2(4):154-160.
[15] Fowler H J,Archer D R.Conflicting signals of climatic change in the upper Indus Basin[J].J Climate,2006,19(17):4276-4293.
[16] Archer D R,Fowler H J.Spatial and temporal variations in precipitation in the upper Indus Basin,global teleconnections and hydrological implications[J].Hydrol Earth Sci Syst,2004,8(1):47-61.