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Glacial response to climate change

A case study

The Tunsberg glacier in Norway, like most of the glaciers around the world, has shown significant ice retreat over the past century. This article looks at research on glacial retreat as evidence of climate change, using the Tunsberg glacier as a case study. It describes survey methods in the field, including the use of GPS and the application of GIS, and is relevant to topics on cold environments and climate change

At the maximum extent of the last (Devensian) glaciation, 20,000 years ago, the whole of Nor way was covered in ice. By about 8,000 years ago, almost all that ice, including most of the areas covered by ice today, had melted. Today Norway’s glaciers cover 2,600 km² — around 1% of the total land area. The Jostedal ice cap, in southern Norway, is the largest ice cap in mainland Europe, covering 487 km² (Figure 1). It started to develop 5,000 years ago, and reached its maximum extent during the Little Ice Age, around 1750, when some valley farms were destroyed by advancing glaciers.

This area is on the same latitude as the southern tip of Greenland, but glaciers exist here not just because of the influence of latitude and altitude. The maritime location results in 1,900 mm of precipitation each year. During the winter months this can fall as up to 2 metres of snow.

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