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Deep-water circulation changes lead North Atlantic climate during deglaciation
Francesco Muschitiello1,2,3, William J D'Andrea4, Andreas Schmittner5
1Department of Geography, University of Cambridge, Cambridge, CB2 3EN, UK. francesco.muschitiello@geog.cam.ac.uk.
Nature Communications
|March 22, 2019
Summary
Changes in North Atlantic Deep Water (NADW) formation precede abrupt climate shifts by about 400 years. This finding improves understanding of climate system response times and predictability.
Area of Science:
- Paleoclimatology
- Climate Dynamics
- Oceanography
Background:
- Understanding the climate system's response time to North Atlantic Deep Water (NADW) formation changes is crucial for climate and Atlantic Meridional Overturning Circulation (AMOC) predictability.
- Previous studies lacked quantitative data on the precise timing between NADW formation shifts and subsequent climate changes.
Purpose of the Study:
- To quantitatively determine the response time of North Atlantic climate to variations in high-latitude NADW formation during the last deglaciation.
- To establish the lead-lag relationship between deep water circulation changes and abrupt climate events.
Main Methods:
- Synchronization of terrestrial, marine, and ice-core records.
- Analysis of a continuous deep water ventilation record from the Nordic Seas.
- Correlation of high-latitude NADW formation rates with Greenland ice core climate records.
Main Results:
- A ~400-year lead of high-latitude NADW formation changes was identified preceding abrupt climate changes in Greenland ice cores.
- This phasing was observed at the onset and end of the Younger Dryas stadial.
- The observed changes are linked to gradual shifts in temperature- and wind-driven freshwater transport.
Conclusions:
- Variations in Nordic Seas deep-water circulation act as precursors to abrupt climate changes.
- Future climate model studies should incorporate and investigate this observed phasing between deep water circulation and climate events.
- This research enhances the predictability of climate and AMOC by clarifying response mechanisms.
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