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首页> 外文期刊>Journal of Hydrology >Recent dynamics of alpine lakes on the endorheic Changtang Plateau from multi-mission satellite data
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Recent dynamics of alpine lakes on the endorheic Changtang Plateau from multi-mission satellite data

机译:多功能卫星数据中高山湖泊高山湖的最新动态

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Highlights ? Fine details of alpine lake dynamics revealed by recent multi-mission images. ? Changes in lake area quantified in both inter-annual and intra-annual scales. ? Changes compared between lake types using three different classifications. ? Mechanisms of revealed lake dynamics explored using climate data. Abstract Monitoring of the alpine lakes on the endorheic Changtang Plateau is vitally important in understanding climate impacts on hydrological cycle. Existing studies have revealed an accelerated lake expansion on the Changtang Plateau during the 2000s compared with prior decades. However, the partial hiatus of recent Landsat archive affected the continuation of understanding the lake changes in the recent decade. Here we synergistically used imagery from Landsat and Huanjing satellites to enable a detailed monitoring of lake area dynamics on the Changtang Plateau. Our results present that lakes on the Changtang Plateau continued to expand at a rapid rate of 340.79km2 yr?1 (1.06% yr?1, p0.05) from 2009 to 2014. Changes in endorheic (terminal) lakes contribute to 98% of the net expansion, suggesting that monitoring endorheic lake dynamics is of critical importance for understanding climate changes. Meanwhile, changes in saline lakes, which are mostly endorheic, account for 96% of the net expansion, implying that the proportion of freshwater storage on the Changtang Plateau is likely in decline. Rapid expansion occurred in both glacier-fed and non-glacier-fed lakes, with a rate of 224.94km2 yr?1 (0.92% yr?1, p0.05) and 115.85km2 yr?1 (1.47% yr?1, p=0.08), respectively, indicating that glacier retreat alone may not fully explain the recent lake expansion. Intra-annual variations of the selected 24 large lakes fluctuated within 0.22–2.46% (in coefficient of variation) for glacier-fed lakes and 0.17–2.36% for non-glacier-fed lakes. Most of these lakes expanded during the unfrozen period (from May/June to October) and reached to their max
机译:<![CDATA [ 亮点 高山湖泊动态的精细细节透露最近的多任务图像 变化湖泊面积定量在两者间的年度内和年度秤 <? CE:对ID = “P0015” 视图= “所有”>相比使用三种不同的分类湖泊类型之间更改 <?CE:对ID = “P0020” 视图= “所有”>揭示湖DYNAM的机制集成电路使用气候数据探索 抽象 上的内流羌塘高原高山湖泊的监测是在水文循环理解气候影响至关重要。现有的研究表明与以前相比,几十年来在2000年期间,在羌塘高原的加速扩湖。然而,最近的陆地卫星存档的局部间断影响的认识在最近十年里湖的变化延续。在这里,我们使用协同从陆地卫星和卫星还精意象,使湖泊面积的动态对羌塘高原的详细监控。我们的结果呈现于羌塘高原湖泊继续在340.79 的快速速率扩大公里 2 1 (1.06%年 1 , p &LT; 0.05)从2009年至2014年的变化内流(终端)湖泊向净扩张的98%,这表明监测内流湖动力是至关重要的了解气候变化。同时,改变咸水湖,其中大多是内流,占净扩张的96%,这意味着淡水储存在羌塘高原的比例可能在下降。迅速膨胀发生在两个冰川喂养和非冰川喂养湖泊,具有224.94的速率公里 2 1 (0.92%年 1 ,p &LT; 0.05)和115.85 公里 2 1 (1.47%年 1 ,p = 0.08),分别指示单靠冰川退缩可能不充分说明近期湖面扩张。所选择的24个大湖泊的帧内年变化0.22-2.46%(在变异系数)为冰川喂养的湖泊和0.17-2.36%的范围内波动,对于非冰川喂养湖泊。大多数这些湖泊在解冻期间(5月/ 6月至10月)扩大,达到其最大

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