{"id":29296,"date":"2026-03-14T18:31:00","date_gmt":"2026-03-14T23:31:00","guid":{"rendered":"https:\/\/www.ecoticias.com\/en\/?p=29296"},"modified":"2026-03-14T09:41:57","modified_gmt":"2026-03-14T14:41:57","slug":"goodbye-to-europes-temperate-climate-if-this-happens-the-model-predicts-drops-of-up-to-10-15-c-in-areas-of-northwestern-europe-after-the-collapse","status":"publish","type":"post","link":"https:\/\/www.ecoticias.com\/en\/goodbye-to-europes-temperate-climate-if-this-happens-the-model-predicts-drops-of-up-to-10-15-c-in-areas-of-northwestern-europe-after-the-collapse\/29296\/","title":{"rendered":"Goodbye to Europe’s temperate climate if this happens: the model predicts drops of up to 10-15 \u00b0C in areas of northwestern Europe after the collapse"},"content":{"rendered":"\n

A powerful Atlantic current<\/a> that helps keep European winters milder than their latitude suggests may be edging toward a critical tipping point, according to a new climate modeling study.<\/p>\n\n\n\n

Scientists say they have, for the first time, simulated a full collapse of this system in a state of the art Earth system model and identified a physical early warning signal that real world observations already show drifting in a worrying direction.<\/p>\n\n\n\n

What is the AMOC and why does it matter?<\/h2>\n\n\n\n

The Atlantic Meridional Overturning Circulation<\/a>, or AMOC, is often compared to a giant conveyor belt in the ocean. It carries warm, salty water from the tropics toward the North Atlantic<\/a> near Europe, where the water cools, becomes denser, sinks and flows back south at depth. That slow overturning helps shape weather patterns, sea level and even rainfall in places as distant as the Amazon and West Africa.<\/p>\n\n\n\n

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If that conveyor weakens too far, northern Europe could see much colder conditions even as the planet as a whole continues to warm<\/a>. Some coastal regions along the Atlantic would also face extra sea level rise on top of the global average.<\/p>\n\n\n\n

Modeling a collapse in slow motion<\/h2>\n\n\n\n

In the new research, a team based at Utrecht University used the Community Earth System Model<\/a> and slowly added fresh water to the North Atlantic surface in a long experiment that ran for more than seventeen hundred simulated years. The extra fresh water makes surface water less salty and less dense, which in turn makes it harder for that water to sink and keep the overturning going.<\/p>\n\n\n\n

For many centuries in the model, the AMOC simply weakened. Then it abruptly collapsed. Northward heat transport in the Atlantic dropped by about three quarters and surface waters around western Europe cooled by up to around ten degrees Celsius. <\/p>\n\n\n\n

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Arctic sea ice expanded far to the south and winter temperatures in several European cities fell by five to fifteen degrees in only about one hundred years, a pace that would be far faster than communities or infrastructure are designed for. That is the kind of shift that would not just nudge your heating bill. It would rewrite what \u201cnormal winter\u201d means.<\/p>\n\n\n\n

A new early warning hiding in salty waters<\/h2>\n\n\n\n

To look for warning signs, the team focused on how the AMOC moves fresh water and salt across the southern boundary of the Atlantic near thirty four degrees south. In simple terms, they tracked whether the overturning current is exporting relatively salty water out of the basin or importing fresher water in.<\/p>\n\n\n\n

In the model, that quantity developed a clear pattern. It became more negative as the system approached instability, then passed through a distinct minimum roughly twenty five years before the simulated collapse. That minimum, together with a rise in year to year variability, acts as a physics-based early warning indicator of an approaching tipping point.<\/p>\n\n\n\n

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Historical reanalysis products, which blend observations with ocean models, already show this same measure trending more negative over the past four decades at a rate of roughly one milli Sverdrup per year. That trend is similar to what high-emission climate scenarios project for the coming century, which is why the authors write that the present day AMOC is \u201con route to tipping.\u201d At the same time, the data record is still too short to say how far away the threshold might be.<\/p>\n\n\n\n

What this means for people and the planet<\/h2>\n\n\n\n

The study does not pin down a calendar year for a real-world collapse. There are known biases in current climate models and the experiment required far more fresh water than the Greenland Ice Sheet is adding today. Yet the work strengthens the case that the AMOC behaves as a true tipping element and that its long-term stability is tightly linked to continued greenhouse gas emissions and ice melt.<\/p>\n\n\n\n

In practical terms, that means two things. Cutting emissions can still reduce the extra fresh water pouring into the North Atlantic in the coming decades. At the same time, keeping and expanding ocean observing arrays<\/a> that monitor this \u201cclimate conveyor belt\u201d will be essential so scientists can spot any real world early warning signal in time.<\/p>\n\n\n\n

The study was published in Science Advances<\/em><\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"

A powerful Atlantic current that helps keep European winters milder than their latitude suggests may be edging toward a critical … <\/p>\n

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