Dansgaard-Oeschger and Heinrich event temperature anomalies in the North Atlantic set by sea ice, frontal position and thermocline structure

We use eighteen timescale-synchronised near-surface temperature reconstructions spanning 10-50 thousand years before present to clarify the regional expression of Dansgaard-Oeschger (D-O) and Heinrich (H) events in the North Atlantic. The North Atlantic Drift region shows D-O temperature variations...

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Bibliographic Details
Main Author: Pedro, J.B. (author)
Other Authors: Andersson, C. (author), Vettoretti, G. (author), Voelker, Antje (author), Waelbroeck, C. (author), Dokken, T.M. (author), Jensen, M.F. (author), Rasmussen, S.O. (author), Sessford, E.G. (author), Jochum, M. (author), Nisancioglu, K.H. (author)
Format: article
Language:eng
Published: 2022
Subjects:
Dansgaard-Oeschger event
Heinrich event
Abrupt climate change
Marine sediment core
Ice core
Sea ice
Online Access:http://hdl.handle.net/10400.1/18117
Country:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/18117

Internet

http://hdl.handle.net/10400.1/18117

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