Ice front blocking in a laboratory model of the Antarctic ice shelf
Mass loss from the Antarctic Ice Sheet to the ocean has increased in recent decades, largely because the thinning of its floating ice shelves has allowed the outflow of grounded ice to accelerate. Enhanced basal melting of the ice shelves is thought to be the ultimate driver of change, motivating a...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
Zenodo
2019
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Subjects: | |
Online Access: | https://dx.doi.org/10.5281/zenodo.3543624 https://zenodo.org/record/3543624 |