Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian
The Eemian period (120 ka) is considered a past analogue for future climatic warming, yet data from the high latitudes remains sparse. Here, the authors show that in Northern Europe, the Eemian saw dramatic climatic shifts, linked to changes in Earth’s orbit and North Atlantic oceanic circulation....
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2018-07-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-018-05314-1 |
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doaj-877d1cb244f94849aeceb599e02b4f192021-01-31T14:50:46ZengNature Publishing GroupNature Communications2041-17232018-07-019111010.1038/s41467-018-05314-1Abrupt high-latitude climate events and decoupled seasonal trends during the EemianJ. Sakari Salonen0Karin F. Helmens1Jo Brendryen2Niina Kuosmanen3Minna Väliranta4Simon Goring5Mikko Korpela6Malin Kylander7Annemarie Philip8Anna Plikk9Hans Renssen10Miska Luoto11Department of Geosciences and Geography, University of HelsinkiDepartment of Physical Geography and the Bolin Centre for Climate Research, Stockholm UniversityDepartment of Earth Science, The Bjerknes Centre for Climate Research, and the Jebsen Centre for Deep Sea Research, University of BergenDepartment of Forest Ecology, Faculty of Forestry and Wood Sciences, Czech University of Life Sciences PragueEnvironmental Change Research Unit (ECRU), Ecosystems and Environment Research Programme, University of HelsinkiDepartment of Geography, University of WisconsinDepartment of Geosciences and Geography, University of HelsinkiDepartment of Geological Sciences and the Bolin Centre for Climate Research, Stockholm UniversityEcosystem and Landscape Dynamics, Institute for Biodiversity and Ecosystem Dynamics, University of AmsterdamDepartment of Physical Geography and the Bolin Centre for Climate Research, Stockholm UniversityDepartment of Natural Science and Environmental Health, University College of Southeast NorwayDepartment of Geosciences and Geography, University of HelsinkiThe Eemian period (120 ka) is considered a past analogue for future climatic warming, yet data from the high latitudes remains sparse. Here, the authors show that in Northern Europe, the Eemian saw dramatic climatic shifts, linked to changes in Earth’s orbit and North Atlantic oceanic circulation.https://doi.org/10.1038/s41467-018-05314-1 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. Sakari Salonen Karin F. Helmens Jo Brendryen Niina Kuosmanen Minna Väliranta Simon Goring Mikko Korpela Malin Kylander Annemarie Philip Anna Plikk Hans Renssen Miska Luoto |
spellingShingle |
J. Sakari Salonen Karin F. Helmens Jo Brendryen Niina Kuosmanen Minna Väliranta Simon Goring Mikko Korpela Malin Kylander Annemarie Philip Anna Plikk Hans Renssen Miska Luoto Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian Nature Communications |
author_facet |
J. Sakari Salonen Karin F. Helmens Jo Brendryen Niina Kuosmanen Minna Väliranta Simon Goring Mikko Korpela Malin Kylander Annemarie Philip Anna Plikk Hans Renssen Miska Luoto |
author_sort |
J. Sakari Salonen |
title |
Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian |
title_short |
Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian |
title_full |
Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian |
title_fullStr |
Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian |
title_full_unstemmed |
Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian |
title_sort |
abrupt high-latitude climate events and decoupled seasonal trends during the eemian |
publisher |
Nature Publishing Group |
series |
Nature Communications |
issn |
2041-1723 |
publishDate |
2018-07-01 |
description |
The Eemian period (120 ka) is considered a past analogue for future climatic warming, yet data from the high latitudes remains sparse. Here, the authors show that in Northern Europe, the Eemian saw dramatic climatic shifts, linked to changes in Earth’s orbit and North Atlantic oceanic circulation. |
url |
https://doi.org/10.1038/s41467-018-05314-1 |
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