The regimes have distinct hydroclimatic spatial imprints, and their occurrence changes are associated with regional trends: WR2 is linked to dynamic temperature trends and fewer cold summer days in Eastern Europe; WR3's increase and WR1's decrease are linked to eastern-European soil-moisture decline; WR1 changes are consistent with western-European soil-moisture trends; and WR2 and WR3 changes are linked to strongest dynamic VPD trends in southern and eastern Europe.

Evidence (1)

European summer drying largely driven by atmospheric circulation changes since the 1980s — Weather-regime changes as mechanisms of circulation-driven drying

The WRs show a clear imprint on the spatial patterns of hydroclimatic variables

https://doi.org/10.1038/s41561-026-02050-w#unit-4-p2

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