Tzedakis_2018_AMOC_slowdown_LIG.png


Summary

Description
English: The North Atlantic climate of the Last Interglacial was affected by the weakening of the Atlantic meridional overturning circulation which had occurred at the time, in terms of sea surface temperature and precipitation .
Date
Source doi : 10.1038/s41467-018-06683-3
Author Tzedakis, P.C., Drysdale, R.N., Margari, V. et al.
Permission
( Reusing this file )
This file, which was originally posted to https://www.nature.com/articles/s41467-018-06683-3 , was reviewed on 19 April 2024 by reviewer Magog the Ogre , who confirmed that it was available there under the stated license on that date.

Licensing

w:en:Creative Commons
attribution
This file is licensed under the Creative Commons Attribution 4.0 International license.
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.

Original upload log

The original description page was here . All following user names refer to en.wikipedia.
Date/Time Dimensions User Comment
2024-04-14 18:19 1333×919× (541118 bytes) InformationToKnowledge This graphic, taken from [https://www.nature.com/articles/s41467-018-06683-3 Tzedakis et al., 2018], shows how the North Atlantic climate of the [[Last Interglacial]] was affected by the weakening of the [[Atlantic meridional overturning circulation]] which had occurred at the time, in terms of [[sea surface temperature]] and [[precipitation]]. Graphic cropped from the left part of [https://www.nature.com/articles/s41467-018-06683-3/figures/6 Figure 6] in the paper.

Captions

Add a one-line explanation of what this file represents

In dieser Datei abgebildete Objekte

depicts