A spatiotemporal reconstruction of sea-surface temperatures in the North Atlantic during Dansgaard-Oeschger events 5-8

• Published in: Aquaculture
• Main Authors: Jensen, Mari F., Nummelin, Aleksi, Nielsen, Soren B., Sadatzki, Henrik, Sessford, Evangeline, Risebrobakken, Bjorg, Andersson, Carin, Voelker, Antje, Roberts, William H. G., Pedro, Joel, Born, Andreas
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications- European Geosciences Union (EGU) 2009
• Subjects: Abrupt climate change; Marine usotope stage-3; Last glacial period; Greenland ice core; Planktonic foraminifera; Coupled climate; Heinrich events; Pmip4 contribution; Ocean circulation; Latitude climate; Greenland; Dansgaard-Oeschger events; ice core; North Atlantic; Sea ice
• Online Access: http://hdl.handle.net/10400.1/11755; https://doi.org/10.1016/j.aquaculture.2009.08.024

Here, we establish a spatiotemporal evolution of the sea-surface temperatures in the North Atlantic over Dansgaard-Oeschger (DO) events 5-8 (approximately 3040 kyr) using the proxy surrogate reconstruction method. Proxy data suggest a large variability in North Atlantic sea-surface temperatures during the DO events of the last glacial period. However, proxy data availability is limited and cannot provide a full spatial picture of the oceanic changes. Therefore, we combine fully coupled, general circulation model simulations with planktic foraminifera based seasurface temperature reconstructions to obtain a broader spatial picture of the ocean state during DO events 5-8. The resulting spatial sea-surface temperature patterns agree over a number of different general circulation models and simulations. We find that sea-surface temperature variability over the DO events is characterized by colder conditions in the subpolar North Atlantic during stadials than during inter-stadials, and the variability is linked to changes in the Atlantic Meridional Overturning circulation and in the sea-ice cover. Forced simulations are needed to capture the strength of the temperature variability and to reconstruct the variability in other climatic records not directly linked to the seasurface temperature reconstructions. This is the first time the proxy surrogate reconstruction method has been applied to oceanic variability during MIS3. Our results remain robust, even when age uncertainties of proxy data, the number of available temperature reconstructions, and different climate models are considered. However, we also highlight shortcomings of the methodology that should be addressed in future implementations. European Research Council under the European Community's Seventh Framework Programme/ERC [610055]; Centre for Climate Dynamics at the Bjerknes Centre