Veille 2.1

Wereldnieuws was het de laatste weken. ‘De Golfstroom kan stilvallen in 2025’, kopten kranten naar aanleiding van een recent verschenen paper. In feite ging de publicatie niet over de Golfstroom, maar over de Atlantic Meridional Overturning Circulation, kortweg AMOC. En bij de genoemde termijn vallen ook vraagtekens te plaatsen. Wat zegt de wetenschap over al die amok rond de AMOC? ‘Of het nu in 2025 is of in 2100, we willen niet dat dit gebeurt.’

The Atlantic meridional overturning circulation (AMOC) is a major tipping element in the climate system and a future collapse would have severe impacts on the climate in the North Atlantic region. In recent years weakening in circulation has been reported, but assessments by the Intergovernmental Panel on Climate Change (IPCC), based on the Climate Model Intercomparison Project (CMIP) model simulations suggest that a full collapse is unlikely within the 21st century. Tipping to an undesired state in the climate is, however, a growing concern with increasing greenhouse gas concentrations. Predictions based on observations rely on detecting early-warning signals, primarily an increase in variance (loss of resilience) and increased autocorrelation (critical slowing down), which have recently been reported for the AMOC. Here we provide statistical significance and data-driven estimators for the time of tipping. We estimate a collapse of the AMOC to occur around mid-century under the current scenario of future emi

The Atlantic Meridional Overturning Circulation (AMOC), a major ocean current system transporting warm surface waters toward the northern Atlantic, has been suggested to exhibit two distinct modes of operation. A collapse from the currently attained strong to the weak mode would have severe impacts on the global climate system and further multi-stable Earth system components. Observations and recently suggested fingerprints of AMOC variability indicate a gradual weakening during the last decades, but estimates of the critical transition point remain uncertain.