Sea ice breakup and marine melt of a retreating tidewater outlet glacier in northeast Greenland (81°N)

Rising temperatures in the Arctic cause accelerated mass loss from the Greenland Ice Sheet and reduced sea ice cover. Tidewater outlet glaciers represent direct connections between glaciers and the ocean where melt rates at the ice-ocean interface are influenced by ocean temperature and circulation....

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Detalles Bibliográficos
Autores principales: Bendtsen, Jørgen, Mortensen, John, Lennert, Kunuk, K. Ehn, Jens, Boone, Wieter, Galindo, Virginie, Hu, Yu-bin, Dmitrenko, Igor A., Kirillov, Sergei A., Kjeldsen, Kristian K., Kristoffersen, Yngve, G. Barber, David, Rysgaard, Søren
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5503942/
https://www.ncbi.nlm.nih.gov/pubmed/28694490
http://dx.doi.org/10.1038/s41598-017-05089-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5503942/
https://www.ncbi.nlm.nih.gov/pubmed/28694490
http://dx.doi.org/10.1038/s41598-017-05089-3

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