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...

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Bibliographic Details
Main Authors: Darelius, Elin, Wahlin, Anna, Steiger, Nadine, Glessmer, Mirjam, Sommeria, Joël, Viboud, Samuel
Format: Dataset
Language:English
Published: Zenodo 2019
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.3543623
https://zenodo.org/record/3543623