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首页> 外文期刊>Environmental Earth Sciences >Glacier No. 4 of Sigong River over Mt. Bogda of eastern Tianshan, central Asia: thinning and retreat during the period 1962–2009
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Glacier No. 4 of Sigong River over Mt. Bogda of eastern Tianshan, central Asia: thinning and retreat during the period 1962–2009

机译:西贡山上的西贡河四号冰川中亚天山东部的博格达:1962-2009年间的减薄和退缩

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摘要

RTK-GPS data, aerial photographs and Aster images were used to quantify volume, surface elevation, terminus position and area changes of Glacier No. 4 of Sigong River over Mt. Bogda, Tianshan during the period from 1962 to 2009. Glacier surface elevation of the tongue area decreased by 15 ± 8 m (0.32 ± 0.17 m a−1) and ice volume loss reached 0.014 ± 0.008 km3 (0.013 ± 0.007 km3 w. e.). The glacier terminus retreated at a rate of 8.0 m a−1 and the area decreased by about 0.53 km2, accounting for 15.8% of the glacier area in 1962 (3.33 km2). The changes can be primarily attributed to the significant increase in temperature in this region. A comparison with glacier changes by field measurements in other regions of eastern Tianshan showed obvious spatial differences in the magnitude of the changes, owing to a combination of regional climate change and topographical factors.
机译:RTK-GPS数据,航拍照片和Aster图像用于量化西贡河上的四公河4号冰川的体积,表面高度,终点位置和面积变化。 1962年至2009年期间,天山博格达。舌头区域的冰川表面海拔降低了15±8 m(0.32±0.17 m a -1 ),冰量损失达到0.014±0.008 km < sup> 3 (0.013±0.007 km 3 w.e。)。冰川终点以8.0 m a -1 的速度退缩,面积减少了约0.53 km 2 ,占1962年冰川面积(3.33 km)的15.8% 2 )。变化主要归因于该区域温度的显着升高。通过将天山东部其他地区的实地测量与冰川变化进行比较,结果表明,由于区域气候变化和地形因素的共同作用,变化幅度存在明显的空间差异。

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