Observed circulation shifts have increased anticyclonic and decreased cyclonic conditions; these conditions favour evapotranspiration through sustained radiation and temperature and reduced rainfall.

Evidence (1)

European summer drying largely driven by atmospheric circulation changes since the 1980s — Problem framing: uncertain dynamic and thermodynamic drivers of European summer drying

Observed shifts in atmospheric circulation have led to more frequent anticyclonic and less frequent cyclonic conditions

https://doi.org/10.1038/s41561-026-02050-w#unit-1-p6

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