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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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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: 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: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2017
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5503942/
https://ncbi.nlm.nih.gov/pubmed/28694490
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-05089-3
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