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Glaciers and global warming

A case study from the High Arctic

This article looks at how glaciers in the High Arctic are responding to global warming, and the likely human impacts. It also explains how analysing these glaciers can help us understand the processes that created UK landforms of glaciation

An actively surging glacier, Comfortlessbreen, in northwest Spitsbergen, Svalbard. The glacier was advancing strongly when this photograph was taken (13 July 2009), soon after which the surge stopped

The High Arctic is a region that is imagined, rather than being strictly defined. Glaciologists tend to think of the region as made up of the numerous islands far north of the Arctic Circle, but Greenland is also included, even though its southern limits are at the latitude of the Shetland Isles.

The High Arctic has glaciers of all types, including the huge Greenland ice sheet, as well as ice caps and highland icefields (where mountains project through the ice). Many of these glaciers are stunningly beautiful, possessing a special character that is quite different from that in the Alps, for example. Yet these glaciers are under threat from the warming climate, and many are no longer being sustained. It could be said they are on borrowed time.

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