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国土资源遥感  2013, Vol. 25 Issue (1): 93-98    DOI: 10.6046/gtzyyg.2013.01.17
  技术应用 本期目录 | 过刊浏览 | 高级检索 |
近20年西昆仑地区冰川动态变化遥感研究
纪鹏1,2, 郭华东1, 张露1
1. 中国科学院对地观测与数字地球科学中心数字地球重点实验室,北京 100094;
2. 上海卫星工程研究所,上海 200240
Remote sensing study of glacier dynamic change in West Kunlun Mountains in the past 20 years
JI Peng1,2, GUO Huadong1, ZHANG Lu1
1. Key Laboratory of Digital Earth, Center for Earth Observation and Digital Earth, Chinese Academy of Sciences, Beijing 100094, China;
2. Shanghai Institute of Satellite Engineering, Shanghai 200240, China
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摘要 

依据西昆仑地区1991—2009年Landsat TM/ETM+遥感图像,获取近20 a西昆仑地区冰川及其冰川融水形成的郭扎错和阿克赛钦湖的动态变化信息,并结合气候资料,分区域综合分析冰川、湖泊变化与气候变化的关系。研究结果表明:1在1991—2009年间,西昆仑冰川有显著变化,但东、西区存在较大差异。其中东区处于先减少,后增加,再减少的波动状态,而西区则处于持续减少状态。与此同时,郭扎错具有先扩大,后缩小,再扩大的变化现象,而阿克赛钦湖则在不断地缩小。2西昆仑冰川与郭扎错、阿克赛钦湖之间,存在着重要的相互作用关系,在数量上成反比。3在2000—2005年间,西昆仑冰川与湖泊面积变化差异产生的主要原因是温度,随着温度的升高,冰川面积减少,湖泊面积增大,三者的变化具有线性关系。

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关键词 社区遥感地学应用灾害响应新技术    
Abstract

Based on the Landsat TM/ETM+ remote sensing images from 1991 to 2009, the authors obtained the dynamic change of the West Kunlun glaciers as well as the Gozha Co and the Aksayqin Lake, with the climatic data, analyzed the change relationship between the glaciers, the lakes and the local climate in different regions. The conclusions of this paper are as follows: 1 In the period of 1991 to 2009, the West Kunlun glaciers were changing obviously, but the east part and the west part show different characteristics. That is, the glaciers of the east part firstly decreased, then increased, and decreased again. The change was fluctuated. However, the situation of the west part was different: the glaciers were decreasing continuously. Meanwhile the Gozha Co was firstly enlarged, then narrowed, and enlarged again while the Aksayqin Lake was narrowed continuously. 2 In the West Kunlun glaciers, there existed important interaction relationship between the Gozha Co and the Aksayqin Lake, showing an inverse ratio in quantity. 3 From 2000 to 2005, the main factor responsible for the difference in area between the West Kunlun glaciers and the lakes was the temperature. With the growing temperature, the area of the glaciers decreased while that of the lakes increased. The variation showed linear relationship.

Key wordscommunity remote sensing(CRS)    geoscience applications    disaster response    new approach
收稿日期: 2011-04-22      出版日期: 2013-02-21
:  TP79  
基金资助:

国家自然科学基金项目(编号:41001268)和973计划项目(编号:2009CB723906)共同资助。

作者简介: 纪鹏(1987-),男,硕士研究生,主要从事全球变化方面的研究。E-mail:advicer_jp@163.com。
引用本文:   
纪鹏, 郭华东, 张露. 近20年西昆仑地区冰川动态变化遥感研究[J]. 国土资源遥感, 2013, 25(1): 93-98.
JI Peng, GUO Huadong, ZHANG Lu. Remote sensing study of glacier dynamic change in West Kunlun Mountains in the past 20 years. REMOTE SENSING FOR LAND & RESOURCES, 2013, 25(1): 93-98.
链接本文:  
https://www.gtzyyg.com/CN/10.6046/gtzyyg.2013.01.17      或      https://www.gtzyyg.com/CN/Y2013/V25/I1/93

[1] 王园香,赵平.GLIMMER 3D陆冰模式及其在青藏高原的应用[J].冰川冻土,2010,32(3):524-531. Wang Y X,Zhao P.A 3D land-ice model GLIMMER and its application in the Tibetan Plateau[J]. Journal of Glaciology and Geocryology,2010,32(3):524-531.

[2] 焦克勤,姚檀栋,李世杰.西昆仑山32 ka来的冰川与环境演变[J].冰川冻土,2000,22(3):250-257. Jiao K Q,Yao T D,Li S J.Evolution of glaciers and environment in the West Kunlun Mountains during the past 32 ka[J].Journal of Glaciology and Geocryology,2000,22(3):250-257.

[3] Paul F, Kääb A,Maisch M,et al.The new remote sensing derived swiss glacier inventory:I methods[J].Annals of Glaciology,2002,34(1):355-361.

[4] 鲁安新,姚檀栋,刘时银,等.青藏高原各拉丹冬地区冰川变化的遥感监测[J].冰川冻土,2002,24(5):559-562. Lu A X,Yao T D,Liu S Y,et al.Glacier change in the Geladandong area of the Tibetan Plateau monitored by remote sensing[J].Journal of Glaciology and Geocryology,2002,24(5):559-562.

[5] 李震,孙文新,曾群柱.综合RS与GIS方法提取青藏高原冰川变化信息——以布喀塔格峰为例[J].地理学报,1999,54(3):263-268. Li Z,Sun W X,Zeng Q Z.Deriving glacier change information on the Xizang (Tibetan) Plateau by integrating RS and GIS techniques[J].Acta Geographica Sinica,1999,54(3):263-268.

[6] 郭华东.中国雷达遥感图像分析[M].北京:科学出版社,1999:87-89. Guo H D.China Radar remote sensing image analysis[M].Beijing:Science Press,1999:87-89.

[7] 上官冬辉,刘时银,丁永建,等.玉龙喀什河源区32年来冰川变化遥感监测[J].地理学报,2004,59(6):855-862. Shangguan D H,Liu S Y,Ding Y J,et al.Glacier changes at the head of Yurungkax River in the west Kunlun Mountains in the past 32 years[J].Acta Geographica Sinica,2004,59(6):855-862.

[8] 张瑞江,赵福岳,方洪宾,等.青藏高原近30年现代雪线遥感调查[J].国土资源遥感,2010,22(s1):59-63. Zhang R J,Zhao F Y,Fang H B,et al.Remote sensing survey of existing snowlines in the past 30 years in Qinghai-Tibet Plateau[J].Remote Sensing for Land and Resources,2010,22(s1):59-63.

[9] 张瑞江,方洪宾,赵福岳,等.青藏高原近30年来现代冰川面积的遥感调查[J].国土资源遥感,2010,22(s1):45-48. Zhang R J,Fang H B,Zhao F Y,et al.Remote sensing survey of existing glaciers in Qinghai-Tibet Plateau[J].Remote Sensing for Land and Resources,2010,22(s1):45-48.

[10] 晋锐,车涛,李新,等.基于遥感和GIS的西藏朋曲流域冰川变化研究[J].冰川冻土,2004,26(3):261-266. Jin R,Che T,Li X,et al.Glacier variation in the Pumqu Basin derived from remote sensing data and GIS technique[J].Journal of Glaciology and Geocryology,2004,26(3):261-266.

[11] 宋波,何元庆,庞洪喜,等.基于遥感和GIS的我国季风海洋型冰川区冰碛物覆盖型冰川边界的自动识别[J].冰川冻土,2007,29(3):456-462. Song B,He Y Q,Pang H X,et al.Identifying automatically the debris-covered glaciers in China's monsoonal temperate-glacier regions based on remote sensing and GIS[J].Journal of Glaciology and Geocryology,2007,29(3):456-462.

[12] Shangguan D H,Liu S Y,Ding Y J,et al.Glacier changes in the west Kunlun Shan from 1970 to 2001 derived from Landsat TM/ETM+ and Chinese glacier inventory data[J].Annals of Glaciology,2007,46(1):204-208.

[13] 纪鹏,郭华东,张露.基于Landsat数据的郭扎错北面冰川近20年来面积动态变化遥感研究[J].遥感技术与应用,2011,26(2):202-208. Ji P,Guo H D,Zhang L.Landsat-based dynamic area change of the glaciers to the north of the Guozhacuo Lake,1991-2009[J].Remote Sensing Technology and Application,2011,26(2):202-208.

[14] 曲耀光,刘景时,马世敏.新疆和田地区的水资源及其潜力[J].干旱区资源与环境,1994,8(2):31-39. Qu Y G,Liu J S,Ma S M.Water resources in Hetian region and the potentialities[J].Journal of Arid Land Resources and Environment,1994,8(2):31-39.

[15] Li X.GLIMS Glacier Database[Z].National snow and ice data center/world data center for glaciology,2003.

[16] 中国大百科全书总编委会.中国大百科全书[M].北京:中国大百科全书出版社,2009. Total Editorial Board of the China Encyclopedia.China encyclopedia[M].Beijing:China Encyclopedia Press, 2009.

[17] 王苏民,窦鸿身.中国湖泊志[M].北京:科学出版社,1998:406. Wang S M,Dou H S.Chinese lake manual[M].Beijing:Science Press,1998:406.

[18] 中科院南京地理与湖泊研究所,中国湖泊数据库[Z].2009. Nanjing Institute of Geography and Limnology,CAS.China lake database[Z].2009.

[19] Kalnay E,Kanamitsu M,Kistler R,et al.The NECP/NCAR 40-year reanalysis project[J].Bull Amer Meteor Soc,1996,77(3):437-471.

[20] 苏志侠,吕世华,罗四维.美国NCEP/NCAR40年全球再分析资料及其解码和图形显示软件简介[J].高原气象,1999,18(2):199-208. Su Z X,Lü S H,Luo S W.NCEP/NCAR 40 years global reanalysis data decoding and graphical display software introduction[J].Plateau Meteorology,1999,18(2):199-208.

[21] Paul F,Kääb A.Perspectives on the production of a glacier inventory from multispectral satellite data in arctic Canada:Cumberland Peninsula,Baffin Island[J].Annals of Glaciology,2005,42(1):59-66.

[22] Tobias B,Brian M,Roger W.Landsat-based inventory of glaciers in western Canada,1985-2005[J].Remote Sensing of Environment,2010,114(1):127-137.

[23] 贾永红.数字图像处理[M].武汉:武汉大学出版社,2003:134. Jia Y H.Digital image processing[M].Wuhan:Wuhan University Press,2004:134.

[24] 周成虎,骆剑承.遥感影像地学理解与分析[M].北京:科学出版社,2003:75-78. Zhou C H,Luo J C.Remote sensing image understanding and analysis[M].Beijing:Science Press,2003:75-78.

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[3] 李进来, 赖吉生. 遥感影像图片制作新技术[J]. 国土资源遥感, 1999, 11(2): 60-62.
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