How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations

Dansgaard-Oeschger events occurred frequently during Marine Isotope Stage 3 (MIS3), as opposed to the following MIS2 period, which included the Last Glacial Maximum (LGM). Transient climate model simulations suggest that these abrupt warming events in Greenland and the North Atlantic region are asso...

Full description

Bibliographic Details
Main Authors: C. J. Van Meerbeeck, H. Renssen, D. M. Roche
Format: Article
Language:English
Published: Copernicus Publications 2009-03-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/5/33/2009/cp-5-33-2009.pdf