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首页> 外文期刊>Journal of Applied Geophysics >Comparison of changes in glacier area and thickness on the northern and southern slopes of Mt. Bogda, eastern Tianshan Mountains
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Comparison of changes in glacier area and thickness on the northern and southern slopes of Mt. Bogda, eastern Tianshan Mountains

机译:山南北坡冰川面积和厚度变化比较。天山东部博格达

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Rapid shrinkage and dramatic volume loss of the glaciers on Mt. Bogda in the eastern Tianshan Mountains have resulted in water shortages in the surrounding arid regions of China. Understanding ice thickness and its variation is important to the analysis of changes in glacial volume, which are directly related to regional hydrology and water resources. Fan-shaped Diffluence Glacier and Heigou Glacier No. 8 are located on the northern and southern slopes of Mt. Bogda, respectively. In this paper, the spatial distribution of the ice thickness of these two glaciers and the changes in their area and volume are discussed based on a 2009 survey result and comparison to previous investigations. The mean ice thickness of the tongue of Fan-shaped Diffluence Glacier was about 823 m and the calculated ice volume was 385.2 x 10(6) m(3) in 2009. It had thinned by 14 +/- 8 m (0.30 +/- 0.17 m a(-1)) from 1962 to 2009, equivalent to an ice volume loss of 65.5 +/- 37.4 x 10(6) m(3). The mean ice thickness of the tongue of Heigou Glacier No. 8 was 58.7 m and the calculated ice volume was 115.1 x 10(6) m(3) in 2009. The tongue of Heigou Glacier No. 8 thinned by 13 6 m (0.57 +/- 0.26 m a(-1)) from 1986 to 2009, which corresponds to an ice volume loss of 25.5 +/- 11.8 x 10(6) m(3). The greater thinning and retreat of Heigou Glacier No. 8 than those of Fan-shaped Diffluence Glacier is partially due to topographic characteristics. The difference can be attributed mainly to the greater increase in temperature on the southern slope than on the northern slope. (C) 2016 Elsevier B.V. All rights reserved.
机译:山顶冰川的快速收缩和巨大的体积损失。天山东部的博格达(Bogda)导致中国周围干旱地区的水资源短缺。了解冰的厚度及其变化对于分析冰川体积的变化非常重要,而冰川体积的变化与区域水文学和水资源直接相关。扇形的Diffluence冰川和黑沟8号冰川位于Mt.博格达分别。本文基于2009年的调查结果并与以往的研究进行了比较,讨论了这两个冰川的冰厚的空间分布及其面积和体积的变化。扇形散流冰川的舌头的平均冰厚约为823 m,2009年计算的冰量为385.2 x 10(6)m(3)。它的厚度减小了14 +/- 8 m(0.30 + / -从1962年到2009年的0.17 ma(-1)),相当于冰量损失65.5 +/- 37.4 x 10(6)m(3)。 2009年,黑沟8号冰川的舌头平均冰厚为58.7 m,计算的冰量为115.1 x 10(6)m(3)。黑沟8号冰川的舌头变薄了13 6 m(0.57从1986年到2009年+/- 0.26 ma(-1)),相当于冰量损失25.5 +/- 11.8 x 10(6)m(3)。黑沟八号冰川的变薄和后退比扇形扩散冰川更大,部分是由于地形特征。造成这种差异的主要原因是南坡的温度比北坡的温度升高更大。 (C)2016 Elsevier B.V.保留所有权利。

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