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...
| Hlavní autoři: | , , , , , , , |
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| Médium: | Článek |
| Jazyk: | English |
| Vydáno: |
Copernicus Publications
2016-07-01
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| Edice: | The Cryosphere |
| On-line přístup: | http://www.the-cryosphere.net/10/1547/2016/tc-10-1547-2016.pdf |