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首页> 外文期刊>Journal of Glaciology >Large surface velocity fluctuations of Biafo Glacier,central Karakoram, at high spatial and temporal resolution from optical satellite images
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Large surface velocity fluctuations of Biafo Glacier,central Karakoram, at high spatial and temporal resolution from optical satellite images

机译:来自喀喇昆仑山脉中部的比亚福冰川的大表面速度波动,来自光学卫星图像的时空分辨率很高

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摘要

Despite global warming and unlike their Himalayan neighbours, glaciers in the Karakoram mountains do not show signs of significant retreat. Here we report high velocity variations of Biafo Glacier, central Karakoram, which occurred between 2001 and 2009 and which indicate considerable dynamics in its flow behaviour. We have generated a dense time series of glacier surface velocities, based on cross-correlation of optical satellite images, which clearly shows seasonal and interannual velocity variations, reaching 50% in some places. The interannual velocity variations resemble the passing of a broad wave of high velocities, with peak velocities during 2005 and some diffusion down-glacier over a period of at least 4 years. High interannual velocity variations are also observed at other glaciers in the vicinity, suggesting a common cause, although these appear to partly comprise longer acceleration phases. Analysis of weather station data provides some indications of meteorological conditions that could have promoted sustained sliding events during this period, but this does not explain the wave-like nature of the acceleration at Biafo Glacier, and the regular, protracted velocity changes.
机译:尽管全球变暖且与喜马拉雅邻国不同,但喀喇昆仑山脉的冰川并未显示出明显的退缩迹象。在这里,我们报告了喀喇昆仑州中部的Biafo冰川的高速变化,该变化发生在2001年至2009年之间,这表明其流动行为具有相当大的动态。根据光学卫星图像的互相关性,我们生成了一个密集的冰川表面速度时间序列,该序列清楚地显示了季节性和年际速度变化,在某些地方达到了50%。年际速度的变化类似于高速的广泛传播,在2005年达到峰值速度,并且在至少4年的时间里有向下扩散的冰川。在附近的其他冰川也观察到较高的年际速度变化,这是一个普遍的原因,尽管这些似乎部分地包括较长的加速阶段。气象站数据的分析提供了一些气象条件的指示,这些气象条件可能在此期间加剧了持续的滑动事件,但这并不能解释Biafo冰川加速的波状性质以及规则的,持续的速度变化。

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