La veille

On why collapse could be much closer than predicted: what happens when the Atlantic Ocean’s heart stops beating?

The Atlantic Meridional Overturning Circulation is the main driver of northward heat transport in the Atlantic Ocean today, setting global climate patterns. Whether global warming has affected the strength of this overturning circulation over the past century is still debated: observational studies suggest that there has been persistent weakening since the mid-twentieth century, whereas climate models systematically simulate a stable circulation. Here, using Earth system and eddy-permitting coupled ocean–sea-ice models, we show that a freshening of the subarctic Atlantic Ocean and weakening of the overturning circulation increase the temperature and salinity of the South Atlantic on a decadal timescale through the propagation of Kelvin and Rossby waves. We also show that accounting for upper-end meltwater input in historical simulations significantly improves the data–model agreement on past changes in the Atlantic Meridional Overturning Circulation, yielding a slowdown of 0.46 sverdrups per decade since 1950

The idea that the AMOC is headed to collapse is very controversial, but it is clearly weakening. If the circulation did collapse, the consequences on both sides of the Atlantic Ocean would be immense—including large changes in temperature and a spike in weather-related disasters.

There is increasing concern that the Atlantic Meridional Overturning Circulation (AMOC) may collapse this century with a disrupting societal impact on large parts of the world. Preliminary estimates of the probability of such an AMOC collapse have so far been based on conceptual models and statistical analyses of proxy data. Here, we provide observationally based estimates of such probabilities from reanalysis data. We first identify optimal observation regions of an AMOC collapse from a recent global climate model simulation. Salinity data near the southern boundary of the Atlantic turn out to be optimal to provide estimates of the time of the AMOC collapse in this model. Based on the reanalysis products, we next determine probability density functions of the AMOC collapse time. The collapse time is estimated between 2037-2064 (10-90% CI) with a mean of 2050 and the probability of an AMOC collapse before the year 2050 is estimated to be 59±17%.

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

Un incendie s'est déclaré mardi dans les dunes près du Brouwersdam dans la province de Hollande méridionale, entrainant l'évacuation de 125 résidents d'un parc de vacances voisin qui ont été relogés dans un hall sportif, rapporte la zone de secours Rotterdam-Rijnmond.

Le typhon Chaba s’est formé au centre de la mer de Chine méridionale et a touché terre samedi après-midi dans le Guangdong.

Les pays asiatiques en bordure de la mer de Chine s’affrontent pour les ressources halieutiques. Une rivalité exacerbée par la raréfaction du poisson et l’accaparement par la Chine des eaux territoriales de la zone.

Les images satellites montrent une augmentation significative de l’apparition de proliférations d’algues dans les zones contestées de la mer de Chine méridionale. Les images suggèrent que ces proliférations d’algues ou cette prolifération de phytoplancton sont liées à la présence de navires ancrés dans la zone et aux activités de construction d’îles dans la région.