Massive subsurface ice formed by refreezing of ice-shelf melt ponds
The influence of surface ponding on the interior of ice shelves is currently unknown. Here, the authors combine surface and borehole geophysics on the Larsen C Ice Shelf, Antarctica, with remote sensing and modelling and show how pond refreezing increases ice shelf density and temperature.
| Main Authors: | , , , , , , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Publishing Group
2016-06-01
|
| Series: | Nature Communications |
| Online Access: | https://doi.org/10.1038/ncomms11897 |