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

Abstract 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 cir...

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Autores principales: Jørgen Bendtsen, John Mortensen, Kunuk Lennert, Jens K. Ehn, Wieter Boone, Virginie Galindo, Yu-bin Hu, Igor A. Dmitrenko, Sergei A. Kirillov, Kristian K. Kjeldsen, Yngve Kristoffersen, David G. Barber, Søren Rysgaard
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/47590520a4bb40d7a576d60fe250c65a
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