Surface buoyancy control of millennial-scale variations in the Atlantic meridional ocean circulation

<p>Dansgaard–Oeschger (DO) events are a pervasive feature of glacial climates. It is widely accepted that the associated changes in climate, which are most pronounced in the North Atlantic region, are caused by abrupt changes in the strength and/or northward extent of the Atlantic meridional o...

Full description

Bibliographic Details
Main Authors: M. Willeit, A. Ganopolski, N. R. Edwards, S. Rahmstorf
Format: Article
Language:English
Published: Copernicus Publications 2024-12-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/20/2719/2024/cp-20-2719-2024.pdf