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CMIP6 Models Predict Significant 21st Century Decline of the Atlantic Meridional Overturning Circulation

Wilbert WeijerLos Alamos National Laboratory Los Alamos NM USAWei ChengJoint Institute for the Study of the Atmosphere and Ocean University of Washington Seattle WA USAOluwayemi A. GarubaPacific Northwest National Laboratory Richland WA USAAixue HuNational Center for Atmospheric Research Boulder, CO USABalasubramanya NadigaLos Alamos National Laboratory Los Alamos NM USA
2020en
ABI

Аннотация

Abstract We explore the representation of the Atlantic Meridional Overturning Circulation (AMOC) in 27 models from the CMIP6 multimodel ensemble. Comparison with RAPID and SAMBA observations suggests that the ensemble mean represents the AMOC strength and vertical profile reasonably well. Linear trends over the entire historical period (1850–2014) are generally neutral, but many models exhibit an AMOC peak around the 1980s. Ensemble mean AMOC decline in future (SSP) scenarios is stronger in CMIP6 than CMIP5 models. In fact, AMOC decline in CMIP6 is surprisingly insensitive to the scenario at least up to 2060. We find an emergent relationship among a majority of models between AMOC strength and 21st century AMOC decline. Constraining this relationship with RAPID observations suggests that the AMOC might decline between 6 and 8 Sv (34–45%) by 2100. A smaller group of models projects much less AMOC weakening of only up to 30%.

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