MIS-11 duration key to disappearance of the Greenland ice sheet
The most pronounced deglaciation of Greenland of the last several hundred thousand years occurred during Marine Isotope Stage 11. Here, the authors show that it was the exceptional duration of the interglacial period that allowed Greenland to melt even though temperatures were only moderately warmer...
Guardado en:
Autores principales: | , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/f1e803d87cfa4985aa27833582bd8be0 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:f1e803d87cfa4985aa27833582bd8be0 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:f1e803d87cfa4985aa27833582bd8be02021-12-02T14:41:59ZMIS-11 duration key to disappearance of the Greenland ice sheet10.1038/ncomms160082041-1723https://doaj.org/article/f1e803d87cfa4985aa27833582bd8be02017-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms16008https://doaj.org/toc/2041-1723The most pronounced deglaciation of Greenland of the last several hundred thousand years occurred during Marine Isotope Stage 11. Here, the authors show that it was the exceptional duration of the interglacial period that allowed Greenland to melt even though temperatures were only moderately warmer than today.Alexander RobinsonJorge Alvarez-SolasReinhard CalovAndrey GanopolskiMarisa MontoyaNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-7 (2017) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q Alexander Robinson Jorge Alvarez-Solas Reinhard Calov Andrey Ganopolski Marisa Montoya MIS-11 duration key to disappearance of the Greenland ice sheet |
description |
The most pronounced deglaciation of Greenland of the last several hundred thousand years occurred during Marine Isotope Stage 11. Here, the authors show that it was the exceptional duration of the interglacial period that allowed Greenland to melt even though temperatures were only moderately warmer than today. |
format |
article |
author |
Alexander Robinson Jorge Alvarez-Solas Reinhard Calov Andrey Ganopolski Marisa Montoya |
author_facet |
Alexander Robinson Jorge Alvarez-Solas Reinhard Calov Andrey Ganopolski Marisa Montoya |
author_sort |
Alexander Robinson |
title |
MIS-11 duration key to disappearance of the Greenland ice sheet |
title_short |
MIS-11 duration key to disappearance of the Greenland ice sheet |
title_full |
MIS-11 duration key to disappearance of the Greenland ice sheet |
title_fullStr |
MIS-11 duration key to disappearance of the Greenland ice sheet |
title_full_unstemmed |
MIS-11 duration key to disappearance of the Greenland ice sheet |
title_sort |
mis-11 duration key to disappearance of the greenland ice sheet |
publisher |
Nature Portfolio |
publishDate |
2017 |
url |
https://doaj.org/article/f1e803d87cfa4985aa27833582bd8be0 |
work_keys_str_mv |
AT alexanderrobinson mis11durationkeytodisappearanceofthegreenlandicesheet AT jorgealvarezsolas mis11durationkeytodisappearanceofthegreenlandicesheet AT reinhardcalov mis11durationkeytodisappearanceofthegreenlandicesheet AT andreyganopolski mis11durationkeytodisappearanceofthegreenlandicesheet AT marisamontoya mis11durationkeytodisappearanceofthegreenlandicesheet |
_version_ |
1718389846623387648 |