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...
Main Authors: | , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Institute of Low Temperature Science, Hokkaido University
|
Subjects: | |
Online Access: | http://hdl.handle.net/2115/45450 |