The thermal regime of sub-polar glaciers mapped by multi-frequency radio-echo sounding
Radio-echo soundings provide an effective tool for mapping the thermal regimes of polythermal glaciers on a regional scale. Radar signals of 320–370 MHz penetrate ice at sub-freezing temperatures but are reflected from the top of layers of ice which are at the melting point and contain water. Radar...
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Published in | Journal of glaciology Vol. 42; no. 140; pp. 23 - 32 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Cambridge, UK
Cambridge University Press
1996
International Glaciological Society |
Subjects | |
Online Access | Get full text |
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