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- W121697555 abstract "In order to make quantitative predictions of the response of glaciers to climatic change it is necessary to have a mathematical model of the many interacting physical processes which occur in the glacial system. One of the most important of these is the transfer of energy between the atmosphere and the upper surface of the glacier. This controls the mass balance of the glacier and, together with dynamical processes, its length and volume. Physics-based “snowmelt” models of mass and energy transfers at a snow or ice-covered surface have been in existence for some time, but they are based on equations for turbulent transfer in the atmosphere which strictly only apply when the underlying sruface is an extensive flat plane and the geostrophic wind is constant in magnitude and direction. Neither of these conditions will generally hold in an alpine glacier valley. This paper discusses how far the physics-based models can be applied in these circumstances." @default.
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- W121697555 date "1989-01-01" @default.
- W121697555 modified "2023-09-28" @default.
- W121697555 title "Energy and Mass Balance Studies in the Firn Area of the Hintereisferner" @default.
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- W121697555 doi "https://doi.org/10.1007/978-94-015-7823-3_21" @default.
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