Lake change and its implication in the vicinity of Mt. Qomolangma (Everest), central high Himalayas, 1970-2009 | |
Wang Zhaofeng; Liu Linshan; Zhang Yili | |
2012 | |
关键词 | Lakes Climate change Shrinkage |
英文摘要 | High-elevation inland lakes are a sensitive indicator of climate change. The extents of lakes in Mt. Qomolangma region have been extracted using the object-based image-processing method providing 6-24 images during 1970-2009. Combined with data from five meteorological stations and three periods' glacier data, the inter-annual and intra-annual lake changes and responses to climate and glacier change have been analyzed. The results show that the lakes have shrunk overall, with clear inter-annual and intra-annual fluctuations during 1970-2009. In general, there appeared a trend of slight shrinkage in the 1970s, distinct shrinkage around 1990, general expansion in 2000 and accelerated decrease after 2000. Lake Peiku and neighboring lakes show a highly consistent change trend (correlation coefficients of 0.68-0.91), with larger lakes having smaller shrinkage rates, which implies a higher stability (in the order of PeikuLangqiangCuochuolong). Lake Peiku, the largest lake, decreased 10.38km2 (3.69% or 0.27km2year-1) during 1970-2009. The changes in Lake Peiku indicate that precipitation is its main source of supply with glacier melt water a key supplement. Meanwhile, Lake Como Chamling reduced by 13.12km2 (19.79%) during 1974-2007, with strong shrinkage-expansion-shrinkage-expansion fluctuations. Overall, lakes in the vicinity of Mt. Qomolangma are a sensitive good indicator to climate change. 2012 Springer-Verlag. |
出处 | Environmental Earth Sciences |
页 | 1-15 |
收录类别 | EI |
语种 | 英语 |
内容类型 | EI期刊论文 |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/27660] |
专题 | 地理科学与资源研究所_历年回溯文献 |
推荐引用方式 GB/T 7714 | Wang Zhaofeng,Liu Linshan,Zhang Yili. Lake change and its implication in the vicinity of Mt. Qomolangma (Everest), central high Himalayas, 1970-2009. 2012. |
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