Extreme deepening of the Atlantic overturning circulation during deglaciation
By S. Barker, G. Knorr, M. Vautravers, P. Diz, L. Skinner. 2010
140 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Environmental Chemistry
View Paper: https://www.semanticscholar.org/paper/4591619897225128576cb61fc2aef268bd8d536a
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In Atmospheric Science
In Environmental Chemistry
Citations in the corpus
- Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling (2018, background): “Analysis of the relative timing of the DO and AIM events was made possible by gas-based ice-core synchronisations (Bender et al., 1994), in particular the fast global variations in atmospheric methane that accompany DO transitions (Blunier et al., 1998; Blunier and Brook, 2001).”
- The last deglaciation: timing the bipolar seesaw (2011, methodology): “Numerical models (e.g. Liu et al., 2009) and recent proxy-based observations from a south Atlantic sediment core (Barker et al., 2010) suggest that the pronounced Bølling warmth was associated with an “overshoot” of the AMOC and a southward expansion of the North Atlantic Deepwater cell.”