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Monitoring lake level changes on the Tibetan Plateau using ICESat altimetry data (2003-2009)

机译:利用ICESat测高数据监测青藏高原的湖泊水位变化(2003-2009)

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In this study, ICESat altimetry data are used to provide precise lake elevations of the Tibetan Plateau (TP) during the period of 2003-2009. Among the 261 lakes examined ICESat data are available on 111 lakes: 74 lakes with ICESat footprints for 4-7. years and 37 lakes with footprints for 1-3. years. This is the first time that precise lake elevation data are provided for the 111 lakes. Those ICESat elevation data can be used as baselines for future changes in lake levels as well as for changes during the 2003-2009 period. It is found that in the 74 lakes (56 salt lakes) examined, 62 (i.e. 84%) of all lakes and 50 (i.e. 89%) of the salt lakes show tendency of lake level increase. The mean lake water level increase rate is 0.23. m/year for the 56 salt lakes and 0.27. m/year for the 50 salt lakes of water level increase. The largest lake level increase rate (0.80. m/year) found in this study is the lake Cedo Caka. The 74 lakes are grouped into four subareas based on geographical locations and change tendencies in lake levels. Three of the four subareas show increased lake levels. The mean lake level change rates for subareas I, II, III, IV, and the entire TP are 0.12, 0.26, 0.19, -0.11, and 0.2. m/year, respectively. These recent increases in lake level, particularly for a high percentage of salt lakes, supports accelerated glacier melting due to global warming as the most likely cause.
机译:在这项研究中,ICESat测高数据用于提供2003-2009年期间青藏高原(TP)的精确湖泊高程。在所检查的261个湖泊中,有111个湖泊具有ICESat数据:74个湖泊的ICESat足迹为4-7。年和37个湖泊,足迹为1-3。年份。这是首次为111个湖泊提供精确的湖泊高程数据。这些ICESat高程数据可以用作未来湖泊水位变化以及2003-2009年期间变化的基准。结果发现,在所检查的74个湖(56个盐湖)中,所有湖中有62个(即84%)盐湖中有50个(即89%)盐湖水位呈上升趋势。湖泊平均水位上升速度为0.23。米/年为56个盐湖和0.27。 50个盐湖的水位增加的米/年。在这项研究中发现的最大湖水位上升速度(0.80 m /年)是Cedo Caka湖。根据地理位置和湖泊水位变化趋势,将74个湖泊分为四个分区。四个分区中的三个显示湖水位上升。 I,II,III,IV和整个TP区域的平均湖泊水位变化率分别为0.12、0.26、0.19,-0.11和0.2。米/年。最近这些湖面水位的上升,特别是对于高比例的盐湖而言,最有可能的原因是全球变暖导致冰川融化加速。

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