Tuesday, June 23, 2009
Ice volume of Switzerland's dwindling glaciers calculated
Science Daily: Swiss glaciers have lost a lot of ice in recent years due to increased melting. As temperatures climb, so do the fears that the glaciers could one day disappear altogether. Until now it could only be estimated approximately how big the ice volume in the Swiss Alps actually is and how it has changed in recent years.
A team of scientists headed by Martin Funk, ETH-Professor at the Laboratory of Hydraulics, Hydrology and Glaciology (VAW) at ETH Zurich, however, has now developed a novel procedure for determining the ice volume of a glacier. Their results are presented in the current issue of Global and Planetary Change.
The researchers developed the new method according to the law of mass conservation, which states that the surface mass balance has to be balanced by the ice flow and the change in ice thickness. This allows [us] to infer on the ice thickness distribution of a glacier from the surface topography by estimating the mass balance distribution. "The calculation of the current ice volume is the most important indicator in predicting future glacier changes," explains Martin Funk.
The scientists applied the procedure to the 59 Swiss glaciers larger than three square kilometers. For the remaining 1’400 glaciers, the ice volume was estimated by using an empirical area-volume approach derived from the new generated data set. The total glacier ice volume in 1999 was estimated to 74 km3, with an accuracy of 9 km3. This means the total volume of all glaciers of Switzerland is smaller than that of the Lake Geneva, which has a water volume of 89 km3. With a glaciated land area of 1’063 km2, the Swiss glaciers have an average ice thickness of 70 meters…..
Lateral moraine on a glacier joining the Gorner Glacier, Zermatt, Switzerland. Taken by Adrian Pingstone in 1963 and released to the public domain.
A team of scientists headed by Martin Funk, ETH-Professor at the Laboratory of Hydraulics, Hydrology and Glaciology (VAW) at ETH Zurich, however, has now developed a novel procedure for determining the ice volume of a glacier. Their results are presented in the current issue of Global and Planetary Change.
The researchers developed the new method according to the law of mass conservation, which states that the surface mass balance has to be balanced by the ice flow and the change in ice thickness. This allows [us] to infer on the ice thickness distribution of a glacier from the surface topography by estimating the mass balance distribution. "The calculation of the current ice volume is the most important indicator in predicting future glacier changes," explains Martin Funk.
The scientists applied the procedure to the 59 Swiss glaciers larger than three square kilometers. For the remaining 1’400 glaciers, the ice volume was estimated by using an empirical area-volume approach derived from the new generated data set. The total glacier ice volume in 1999 was estimated to 74 km3, with an accuracy of 9 km3. This means the total volume of all glaciers of Switzerland is smaller than that of the Lake Geneva, which has a water volume of 89 km3. With a glaciated land area of 1’063 km2, the Swiss glaciers have an average ice thickness of 70 meters…..
Lateral moraine on a glacier joining the Gorner Glacier, Zermatt, Switzerland. Taken by Adrian Pingstone in 1963 and released to the public domain.
Labels:
2009_Annual,
glacier,
science,
Switzerland
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