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首页> 外文期刊>Journal of Glaciology >The evolution of Fedchenko glacier in the Pamir, Tajikistan, during the past eight decades
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The evolution of Fedchenko glacier in the Pamir, Tajikistan, during the past eight decades

机译:过去八十年来塔吉克斯坦帕米尔的Fedchenko冰川的演变

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摘要

Fedchenko glacier is by far the largest glacier in the Pamir, Tajikistan. Owing to early accurate mapping of the glacier it is possible to evaluate glacier changes over eight decades, which is an exceptionally long time period for this remote mountain region. During this time a total volume loss of 5 km3 was observed on the main trunk of the glacier, while the total area changed by only 1.4%. It is observed that the volume loss migrates from the lower parts of the glacier towards the upper ablation zone. The comparatively small change in area is a result of the supraglacial debris cover on the glacier tongue, which decouples the area loss from the volume loss to a considerable degree. The observed velocities of the glacier do not reflect the volume changes up to now because the interannual variability is larger than possible long-term changes so far. The intra-annual velocity distribution in the central ablation zone probably reflects the evolution of the basal drainage system. Based on ice thickness measurements and simple ice-dynamic assumptions, the total volume of Fedchenko glacier is 123.4 ±28 km~3.
机译:费德琴科冰川是塔吉克斯坦帕米尔最大的冰川。由于早期对冰川进行了精确的制图,因此有可能评估八十年来的冰川变化,这对于这个偏远的山区来说是一个非常长的时期。在这段时间内,冰川主干道的总体积损失为5 km3,而总面积仅变化了1.4%。可以看到,体积损失从冰川的下部向上部的消融区迁移。面积相对较小的变化是冰川舌上的冰川碎屑覆盖造成的,这在很大程度上将面积损失与体积损失脱钩。由于年际变化大于到目前为止可能发生的长期变化,因此观测到的冰川速度至今尚未反映出体积变化。中央消融区的年内速度分布可能反映了基础引流系统的演变。根据冰层厚度的测量和简单的冰动力学假设,费琴科冰川的总体积为123.4±28 km〜3。

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