Interplay of grounding-line dynamics and sub-shelf melting during retreat of the Bjørnøyrenna Ice Stream

The Barents Sea Ice Sheet was a marine-based ice sheet, i.e., it rested on the Barents Sea floor during the Last Glacial Maximum (21 ky BP). The Bjørnøyrenna Ice Stream was the largest ice stream draining the Barents Sea Ice Sheet and is regarded as an analogue for contemporary ice streams in West A...

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Publicado no:Sci Rep
Main Authors: Petrini, Michele, Colleoni, Florence, Kirchner, Nina, Hughes, Anna L. C., Camerlenghi, Angelo, Rebesco, Michele, Lucchi, Renata G., Forte, Emanuele, Colucci, Renato R., Noormets, Riko
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5940849/
https://ncbi.nlm.nih.gov/pubmed/29740089
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-25664-6
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