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Anthropogenic AMOC-temperature drop
The previously predicted regional Northern temperature drop from anthropogenic freshwater-induced AMOC weakening is found counterbalanced by the warming contributions from CO2 and ice melt.openaire +1 more source
On the detectability of multi-centennial AMOC variations
Understanding natural variability in the strength of the Atlantic Meridional Overturning Circulation (AMOC) on centennial to multi-centennial timescales is important in the light of recent AMOC changes, as well as predicted future changes. However, AMOC variability simulated by climate models varies widely in both characteristics and underlying ...Pepijn Bakker +3 more
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120 Years of AMOC Variability Reconstructed From Observations Using the Bernoulli Inverse
Geophysical Research Letters, 2021Stuart Cunningham, Fraser Neil
exaly
Aerosol-Forced AMOC Changes in CMIP6 Historical Simulations
Geophysical Research Letters, 2020Laura J. Wilcox +2 more
exaly
AMOC tipping risk reconsidered
The AMOC is crucial and sensitive part of the global climate system. It transports huge amounts of heat north across the equator into the northern Atlantic. It is the main reason why the Northern Hemisphere is 1 – 2 °C warmer than the Southern Hemisphere (Feulner et al.openaire +1 more source
Fingerprinting the AMOC and predicting a collapse
 In a recent paper [2] we predicted a collapse of the AMOC as soon as mid-century at odds with assessments based on climate model scenarios. The prediction was based on the sub polar gyre fingerprint as a proxy for the AMOC as proposed by Ceasar et al. [2].openaire +1 more source
The effect of model bias on Atlantic freshwater transport and implications for AMOC bi-stability
Tellus, Series A: Dynamic Meteorology and Oceanography, 2022exaly
Irminger Sea Is the Center of Action for Subpolar AMOC Variability
Geophysical Research Letters, 2022Sheldon Bacon +2 more
exaly
Latitudinal dependence of Atlantic meridional overturning circulation (AMOC) variations
Geophysical Research Letters, 2010Rong Zhang
exaly

