Retreat of the glaciers

Earth's glaciers are melting - and not just since the hundred-year summer in 2003. Since the end of the 19th century, in fact, the entire glacial surface of the Alps has shrunk by about 30 to 40%, and worldwide by a staggering 50%.

Often referred to as the earth's "thermometer", these ice colossuses have thus reacted to the 0.7°C rise in the global mean temperature over the same period. Although large parts of the Alps have been ice-free several times since the end of the last cold period some 10,000 years ago - most recently during Roman times - the latter-day glacier retreat is having a considerably greater impact on humans, because the Alps are much more densely populated nowadays. And the foothills, too, are now increasingly dependent on hydrological processes in the highlands.

Water balance

Glaciers have an important compensatory effect on the water balance in the mountains and their foothills: in high precipitation years, more water is retained, since the snow cover accumulating on glaciers protects the ice from melting. In warmer and drier years, glaciers offset the lower precipitation amounts with a higher meltwater input.

If the glaciers disappear, this compensatory effect will be lost as well; the seasonal fluctuations in run-off will no longer be balanced out in the lowlands. In the summer of 2004, 90% of the water at the mouth of the Rhine on the North Sea had already been in the river at Basle, and 50% of that was meltwater from ice and snow.

Low water levels not only impede shipping but also increase pollutant concentrations in rivers. Factories are forced to cut production in order to adhere to pollution thresholds. Hydropower stations generate less electricity, while nuclear power plants are unable to withdraw sufficient cooling water from rivers. Last but not least the water table is falls, which may have far-reaching effects not only on the flora but also on the production and replenishment of drinking water.

The situation is even more dramatic in the earth's arid zones: 70% of the water in the Ganges, for example, stems from Nepalese rivers which are mostly fed by meltwater. Nearly all of the water in Lake Aral comes from the glaciers of the Tien Shan and Pamir mountains.

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