Is the Atlantic Overturning Circulation approaching a tipping point? ...
<!--!introduction!--> Possible changes in Atlantic meridional overturning circulation (AMOC) provide a key source of uncertainty regarding future climate change. Maps of temperature trends over the twentieth century show a conspicuous region of cooling in the northern Atlantic, as well as exce...
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Format: | Conference Object |
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GFZ German Research Centre for Geosciences
2023
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Online Access: | https://dx.doi.org/10.57757/iugg23-0691 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016797 |
Summary: | <!--!introduction!--> Possible changes in Atlantic meridional overturning circulation (AMOC) provide a key source of uncertainty regarding future climate change. Maps of temperature trends over the twentieth century show a conspicuous region of cooling in the northern Atlantic, as well as excessive warming along the North American coast. Both combined are a ‘fingerprint’ characteristic of an AMOC slowdown by about 15%. Proxy data studies suggest this slowing of the AMOC is unique in the past millennium or more. Continued melting of the Greenland Ice Sheet in the coming decades could contribute to further weakening of the AMOC, with important consequences for the ocean ecosystem, the weather in the wider North Atlantic region, regional sea levels and the ocean’s ability to absorb carbon dioxide. Moreover, the AMOC has a known tipping point. The question of how close we already are to this tipping point is becoming increasingly urgent. Rahmstorf, S., et al. (2015). "Exceptional twentieth-century slowdown ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
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