Articles | Volume 2, issue 1
https://doi.org/10.5194/wcd-2-163-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-2-163-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A regime view of future atmospheric circulation changes in northern mid-latitudes
Institute of Atmospheric Sciences and Climate (ISAC-CNR), Bologna, Italy
Virna L. Meccia
Institute of Atmospheric Sciences and Climate (ISAC-CNR), Bologna, Italy
Paolo Davini
Institute of Atmospheric Sciences and Climate (ISAC-CNR), Turin, Italy
Paolo Ghinassi
Institute of Atmospheric Sciences and Climate (ISAC-CNR), Bologna, Italy
Susanna Corti
Institute of Atmospheric Sciences and Climate (ISAC-CNR), Bologna, Italy
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- Impacts of a weakened AMOC on precipitation over the Euro-Atlantic region in the EC-Earth3 climate model K. Bellomo et al. 10.1007/s00382-023-06754-2
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- How Do Stratospheric Perturbations Influence North American Weather Regime Predictions? S. Lee et al. 10.1175/JCLI-D-21-0413.1
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Latest update: 20 Nov 2024
Short summary
Global warming not only affects the mean state of the climate (i.e. a warmer world) but also its variability. Here we analyze a set of future climate scenarios and show how some configurations of the wintertime atmospheric flow will become more frequent and persistent under continued greenhouse forcing. For example, over Europe, models predict an increase in the NAO+ regime which drives intense precipitation in northern Europe and the British Isles and dry conditions over the Mediterranean.
Global warming not only affects the mean state of the climate (i.e. a warmer world) but also its...