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青藏高原热融湖塘动态监测中高分辨率遥感数据处理方法研究
引用本文:王慧妮,刘海松,董晟,倪万魁,林战举.青藏高原热融湖塘动态监测中高分辨率遥感数据处理方法研究[J].冰川冻土,2013,35(1):164-170.
作者姓名:王慧妮  刘海松  董晟  倪万魁  林战举
作者单位:1. 长安大学地测学院,陕西西安710054;中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室,甘肃兰州 730000
2. 北京工业大学建筑工程学院,北京,100124
3. 长安大学地测学院,陕西西安,710054
4. 中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室,甘肃兰州,730000
基金项目:国家自然科学重点基金项目,国家重点基础研究发展计划(973计划)项目,中国科学院西部行动计划项目,国家自然科学创新群体项目
摘    要:遥感技术由于能够快速、 宏观的获得研究区域的数据, 已成为青藏高原热融湖塘动态监测的重要技术手段. 基于野外现场调查和SPOT-5、 QuickBird两种高分辨率遥感卫星数据的特性分析, 结合影响青藏高原热融湖塘发育的一系列特征因素, 探讨了最适合于青藏高原热融湖塘动态监测的高分辨率遥感数据的纠正、 融合和信息提取方法. 应用该方法对2006—2009年间北麓河盆地北侧的红梁河至秀水河段公路沿线局部63 km2范围的热融湖塘进行了变化特征分析, 结果表明该区的热融湖塘个数和总面积在研究时段都有所增加, 其中湖塘由70个增加到75个, 湖塘总面积增量19.65%.

关 键 词:多年冻土  热融湖塘  遥感影像  融合  信息提取  
收稿时间:2012-08-27

Processing Method of High Spatial Resolution Remote Sensing Data in Dynamic Monitoring the Thermokarst Lakes in the Tibetan Plateau
WANG Hui-ni,LIU Hai-song,DONG Sheng,NI Wan-kui,LIN Zhan-ju.Processing Method of High Spatial Resolution Remote Sensing Data in Dynamic Monitoring the Thermokarst Lakes in the Tibetan Plateau[J].Journal of Glaciology and Geocryology,2013,35(1):164-170.
Authors:WANG Hui-ni  LIU Hai-song  DONG Sheng  NI Wan-kui  LIN Zhan-ju
Institution:1. College of Geology Engineering and Geomatics, Changan University, Xi'an Shaanxi 710054, China;
2. State Key Laboratory of Frozen Soil Engineering, Cold and Arid Regions Environmental and Engineering Research Institute, Lanzhou Gansu 730000, China;
3. The College of Architecture and Civil Engineering, Beijing University of Technology, Beijing 100124, China
Abstract:Remote sensing technology has become an important tool to dynamically monitor the processes of thermokarst lakes in the Tibetan Plateau, from which macroscopical spatial data can be obtained rapidly. In this work, the data processing methods including data correcting, data fusion and information extraction were proposed and discussed based on the characteristics of the high spatial resolution remote sensing data from QuickBird and SPOT-5, combining with character factors of the thermokarst lakes in the Qinghai-Tibet Plateau. Furthermore, a most suitable procedure was applied to investigate the change of the thermokarst lakes in a limited range, 63 km2 in area, located in the north of the Beiluhe River basin from 2006 to 2009. The area is from Honglianghe to Xiushuihe along the Qinghai-Tibet Highway. The results show that the amount and total area of the thermokarst lakes have slightly increased.
Keywords:permafrost  thermokarst lake  remote sensing image  fusion  information extraction
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