Abstract
Between 2003 and 2007, North Gasherbrum Glacier on the northeastern slope of the Karakoram mountains in Asia underwent a dramatic acceleration, during which a velocity wave propagated down the glacier. There was a significant transfer of ice from up-glacier downstream, which resulted in a strong surface elevation increase over the lower tongue, but only a moderate advance of the glacier snout. We interpret this behaviour as that of a glacier surge, and we explain the observations by means of a simple version of the Kamb drainage-switching theory.
| Original language | English |
|---|---|
| Pages (from-to) | 904-916 |
| Number of pages | 13 |
| Journal | Journal of Glaciology |
| Volume | 57 |
| Issue number | 205 |
| DOIs | |
| Publication status | Published - Oct 2011 |
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