Articles | Volume 2, issue 1
Weather Clim. Dynam., 2, 163–180, 2021
Weather Clim. Dynam., 2, 163–180, 2021

Research article 10 Mar 2021

Research article | 10 Mar 2021

A regime view of future atmospheric circulation changes in northern mid-latitudes

Federico Fabiano et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Federico Fabiano on behalf of the Authors (13 Jan 2021)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (26 Jan 2021) by Thomas Birner
RR by Anonymous Referee #1 (29 Jan 2021)
RR by Anonymous Referee #2 (02 Feb 2021)
ED: Publish subject to technical corrections (04 Feb 2021) by Thomas Birner
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.