An ice-sheet-wide framework for englacial attenuation from ice-penetrating radar data
Radar inference of the bulk properties of glacier beds, most notably identifying basal melting, is, in general, derived from the basal reflection coefficient. On the scale of an ice sheet, unambiguous determination of basal reflection is primarily limited by uncertainty in the englacial attenuation...
| Main Authors: | , , , , , , , |
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| 格式: | 文件 |
| 语言: | English |
| 出版: |
Copernicus Publications
2016-07-01
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| 丛编: | The Cryosphere |
| 在线阅读: | http://www.the-cryosphere.net/10/1547/2016/tc-10-1547-2016.pdf |