{"id":107073,"date":"2025-05-21T09:07:52","date_gmt":"2025-05-21T07:07:52","guid":{"rendered":"https:\/\/www.sonnenseite.com\/?p=107073"},"modified":"2025-05-21T09:07:53","modified_gmt":"2025-05-21T07:07:53","slug":"glaciers-will-take-centuries-to-recover-even-if-global-warming-is-reversed-scientists-warn","status":"publish","type":"post","link":"https:\/\/www.sonnenseite.com\/en\/environment\/glaciers-will-take-centuries-to-recover-even-if-global-warming-is-reversed-scientists-warn\/","title":{"rendered":"Glaciers will take centuries to recover even if global warming is reversed, scientists warn"},"content":{"rendered":"\n

New research reveals mountain glaciers across the globe will not recover for centuries \u2013 even if human intervention cools the planet back to the 1.5\u00b0C limit, having exceeded it.<\/p>\n\n\n\n

The research<\/a>, led by the University of Bristol in the UK and the University of Innsbruck in Austria, presents the first global simulations of glacier change up to 2500 under so-called \u2018overshoot\u2019 scenarios, when the planet temporarily exceeds the 1.5\u00b0C limit up to 3\u00b0C before cooling back down.<\/p>\n\n\n\n

The results, published today in Nature Climate Change<\/em>, show that such a scenario could result in glaciers losing up to 16% more of their mass compared to a world that never crosses the 1.5\u00b0C threshold.<\/p>\n\n\n\n

Corresponding author Dr Fabien Maussion, Associate Professor in Polar Environmental Change at the University of Bristol, said: \u201cCurrent climate policies are putting the Earth on a path close to 3\u00b0C. It\u2019s clear that such a world is far worse for glaciers than one where the 1.5\u00b0C limit is held.<\/p>\n\n\n\n

\u201cWe aimed to discover whether glaciers can recover if the planet cools again. It\u2019s a question many people ask\u2014will glaciers regrow in our lifetime, or that of our children? Our findings indicate sadly not.\u201d<\/p>\n\n\n\n

Rising global temperatures now indicate a significant chance of overshooting of the Paris Agreement limits adopted a decade ago. For example, last year was the hottest year<\/a> ever recorded on Earth and the first calendar year to exceed the 1.5\u00b0C mark.<\/p>\n\n\n\n

The climate scientists assessed future glacier evolution under a strong overshoot scenario in which global temperatures continue rising to 3.0\u00b0C by around 2150, before falling back to 1.5\u00b0C by 2300 and stabilising. This scenario reflects a delayed net-zero future, in which negative emission technologies like carbon capture are only deployed after critical warming thresholds have been exceeded.<\/p>\n\n\n\n

The results show glaciers would fare much worse than in a world where temperatures stabilise at 1.5\u00b0C without overshooting, with an additional 16% of glacier mass being lost by 2200, and 11% more by 2500 \u2013 on top of the 35% already committed to melting even at 1.5\u00b0C<\/a>. This extra meltwater eventually reaches the ocean, contributing to even greater sea-level rise.<\/p>\n\n\n\n

The research used a pioneering open-source model<\/a> developed at the University of Bristol and partner institutions, which simulates past and future changes in all of the world\u2019s glaciers, excluding the two polar ice sheets. It was combined with novel global climate projections produced by the University of Bern in Switzerland.<\/p>\n\n\n\n

Lead author Dr Lilian Schuster, a researcher at the University of Innsbruck, said: \u201cOur models show it would take many centuries, if not millennia, for the large polar mountain glaciers to recover from a 3\u00b0C overshoot. For smaller glaciers such as those in the Alps, the Himalaya and the Tropical Andes, recovery won\u2019t be seen by the next generations but is possible by 2500.\u201d<\/p>\n\n\n\n

Glacier meltwater in these mountain regions is vital to downstream communities \u2013 especially during dry seasons. When glaciers melt, they temporarily release more water, a phenomenon known as glacier \u2018peak water\u2019.<\/p>\n\n\n\n

Dr Schuster added: \u201cIf glaciers regrow, they start storing water again as ice \u2013 and that means less water flows downstream. We call this effect \u2018trough water\u2019, in contrast to peak water. We found that roughly half of the basins we studied will experience some form of trough water beyond 2100. It\u2019s too early to say how much impact this will have, but our study is a first step toward understanding the many and complex consequences of climate overshoots for glacier-fed water systems and sea-level rise.\u201d<\/p>\n\n\n\n

This research was conducted as part of the EU-funded PROVIDE<\/a> project, which investigates the impacts of climate overshoots on key sectors around the world.<\/p>\n\n\n\n

Dr Maussion said: \u201cOvershooting 1.5\u00b0C, even temporarily, locks in glacier loss for centuries. Our study shows that much of this damage cannot simply be undone \u2013 even if temperatures later return to safer levels. The longer we delay emissions cuts, the more we burden future generations with irreversible change.\u201d<\/p>\n\n\n\n