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...
| Κύριοι συγγραφείς: | , , , , , , , |
|---|---|
| Μορφή: | Άρθρο |
| Γλώσσα: | English |
| Έκδοση: |
Copernicus Publications
2016-07-01
|
| Σειρά: | The Cryosphere |
| Διαθέσιμο Online: | http://www.the-cryosphere.net/10/1547/2016/tc-10-1547-2016.pdf |