Geodetic measurements reveal similarities between post–Last Glacial Maximum and present-day mass loss from the Greenland ice sheet

Accurate quantification of the millennial-scale mass balance of the Greenland ice sheet (GrIS) and its contribution to global sea-level rise remain challenging because of sparse in situ observations in key regions. Glacial isostatic adjustment (GIA) is the ongoing response of the solid Earth to ice...

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Detalles Bibliográficos
Autores principales: Khan, Shfaqat A., Sasgen, Ingo, Bevis, Michael, van Dam, Tonie, Bamber, Jonathan L., Wahr, John, Willis, Michael, Kjær, Kurt H., Wouters, Bert, Helm, Veit, Csatho, Beata, Fleming, Kevin, Bjørk, Anders A., Aschwanden, Andy, Knudsen, Per, Munneke, Peter Kuipers
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5031466/
https://www.ncbi.nlm.nih.gov/pubmed/27679819
http://dx.doi.org/10.1126/sciadv.1600931

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5031466/
https://www.ncbi.nlm.nih.gov/pubmed/27679819
http://dx.doi.org/10.1126/sciadv.1600931

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