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Brief Communication: Further summer speedup of Jakobshavn Isbræ

机译:简讯:雅各布·伊斯布雷的夏季进一步提速

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摘要

We have extended the record of flow speed on Jakobshavn Isbræ through the summer of 2013. These new data reveal large seasonal speedups, 30 to 50% greater than previous summers. At a point a few kilometres inland from the terminus, the mean annual speed for 2012 is nearly three\udtimes as great as that in the mid-1990s, while the peak summer speeds are more than a factor of four greater. These speeds were achieved as the glacier terminus appears to have retreated to the bottom of an over-deepened basin with a depth of ~1300m below sea level. The terminus is likely to reach the deepest section of the trough within a few decades, after which it could rapidly retreat to the shallower regions ~50 km farther upstream, potentially by the end of this century.
机译:我们将JakobshavnIsbræ的水流速度记录延长至2013年夏季。这些新数据显示,季节性季节性水流明显增加,比以前的夏季增加30%至50%。在距离终点站内陆几公里处,2012年的年平均速度几乎是1990年代中期的三倍,而夏季的最高时速则高出四倍。这些速度之所以能够达到,是因为冰川终点似乎已退缩到一个超深盆地的底部,该盆地的深度低于海平面约1300m。总站很可能在几十年内到达海槽的最深部分,此后它可能迅速撤退到更上游约50公里的较浅区域,可能在本世纪末。

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