Impact of Local Insolation on Snow Metamorphism and Ice Core Records

Local insolation is a major component of the energy balance at the surface of an ice sheet and causes temperature gradient metamorphism (TGM) of snow and firn. TGM is one of the dominant processes changing the structure of dry snow. We present a physically based model that calculates insolation-indu...

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Bibliographic Details
Main Authors: Hutterli, Manuel A., Schneebeli, Martin, Freitag, Johannes, Kipfstuhl, Josef, Röthlisberger, Regine
Format: Article in Journal/Newspaper
Language:English
Published: Institute of Low Temperature Science, Hokkaido University
Subjects:
400
Online Access:http://hdl.handle.net/2115/45450