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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5940849/
https://www.ncbi.nlm.nih.gov/pubmed/29740089
http://dx.doi.org/10.1038/s41598-018-25664-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5940849/
https://www.ncbi.nlm.nih.gov/pubmed/29740089
http://dx.doi.org/10.1038/s41598-018-25664-6

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