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20th-century glacier fluctuations on Disko Island (Qeqertarsuaq), Greenland

机译:格陵兰岛(QEQERTARSUAQ)的20世纪冰川波动

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This study assesses glacier fluctuations on Disko Island (Qeqertarsuaq), central West Greenland, during the 20th century. A total of 247 glaciers, of which 75 are classified as surge-type glaciers, are included, representing about 95% of the glacierized area. Based on expedition accounts and early maps, it is concluded that recession rates were highest during the first half of the century. Between 1953 and 2005, 70% of the glaciers showed recession, 28% remained stationary and 2% experienced overall advance due to glacier surging. The mean recession rate of quiescent surge-type glaciers was 20 m a?1 compared to 8 m a?1 for normal glaciers. Identification of changes in glacier length controlled by climate changes is achieved by excluding surge-type glaciers from the dataset. The result indicates that glaciers with ablation areas facing in the arc south to northwest, covering an area above 5 km2 and having a terminus elevation below 800 m are the most climate-sensitive.
机译:本研究评估了20世纪格陵兰州的Disko Island(Qeqertarsuaq)的冰川波动。共有247个冰川,其中75个被归类为电涌型冰川,包括约95%的冰川化区域。基于探险账户和早期地图,得出结论,该世纪上半叶的衰退率最高。 1953年至2005年间,70%的冰川表现出衰退,28%仍然是普通的,2%由于冰川飙升而经历了总体进步。静态喘级冰川的平均衰退率为20米A?1与普通冰川的8米A?1相比。通过从数据集中排除电涌型冰川来实现气候变化控制的冰川长度的变化。结果表明,冰川与面向西北部的弧形到西北部的消融区域,覆盖5 km 2以上的面积并具有低于800米以下的末端升高是最具气候敏感的。

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