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作 者:乔程[1,4] 骆剑承[1] 盛永伟 沈占锋[1] 李均力[3] 郜丽静[1]
机构地区:[1]中国科学院遥感应用研究所,北京100101 [2]Department of Geography,UCLA,CA90095-1524 [3]中国科学院新疆生态与地理研究所,乌鲁木齐830011 [4]中国科学院研究生院,北京100049
出 处:《湖泊科学》2010年第1期98-102,共5页Journal of Lake Sciences
基 金:国家重点基础研究发展计划(863)项目(2009AA12Z123);国家自然科学基金项目(40871203);NASA New InvestigatorProgram(NNX06AE58G)联合资助
摘 要:青藏高原湖泊受人类活动干扰较少,主要受气候变化导致的冰川融化和蒸发的影响,是气候变化直观敏感的反映区。因此,研究青藏高原湖泊变化对区域以至全球气候、环境变化的研究具有深远意义。本文在遥感影像的基础上发展了综合指数计算与空间分异的现存湖迭代提取方法,对影像数据上的湖泊进行动态监测;并结合DEM数据发展了半自动化的古岸线提取方法,进而分析古湖泊的变化,二者相结合直观全面地反映出了青藏高原湖泊的古今变化情况。并以达则错湖为例进行提取。Lakes on the Tibetan Plateau, which are rarely influenced by disturbance of human activities and mainly controlled by glacier melting and evaporation caused by climate change, are a typical study area of global climate and environment change. Remote sensing technology to monitor lake changes across the plateau has important significance to global climate and environment change research. This paper developed an iterative modem lake extraction method on remote sensing images using index calculation and spatial difference comprehensively, to detect lake changes dynamically ; and developed a semi-automatic paleo-shoreliue extraction method combined with DEM, so as to analyze paleo-lake change. Combining the two methods, we can clearly and completely get the lake changes across the Tibetan Plateau since the ancient and modem ages. Finally, we took Dagze Co as an example to proceed with the methods, and analyzed its shrinkage conditions since the latest 25 years and since the Great Lake Period.
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