Grounding-line basal melt rates determined using radar-derived internal stratigraphy
We use ice-penetrating radar data across grounding lines of Siple Dome and Roosevelt Island, Antarctica, to measure the spatial pattern, magnitude and duration of sub-ice-shelf melting at these locations. Stratigraphic layers across the grounding line show, in places, a large-amplitude downwarp at,...
Main Authors: | , , |
---|---|
Format: | Text |
Language: | unknown |
Published: |
PDXScholar
2010
|
Subjects: | |
Online Access: | https://pdxscholar.library.pdx.edu/geology_fac/22 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1021&context=geology_fac |