Radar attenuation demonstrates advective cooling in the Siple Coast ice streams

Ice streams are warmed by shear strain, both vertical shear near the bed and lateral shear at the margins. Warm ice deforms more easily, establishing a positive feedback loop in an ice stream where fast flow leads to warm ice and then to even faster flow. Here, we use radar attenuation measurements...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Hills, Benjamin H., Christianson, Knut, Jacobel, Robert W., Conway, Howard, Pettersson, Rickard
Format: Article in Journal/Newspaper
Language:English
Published: Uppsala universitet, Luft-, vatten- och landskapslära 2022
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-510584
https://doi.org/10.1017/jog.2022.86