Soil moisture declines by −0.41 mm per decade in HIST and −0.23 mm per decade in NAT, implying a 55% dynamic contribution.

Evidence (1)

European summer drying largely driven by atmospheric circulation changes since the 1980s — Partitioning post-1980 hydroclimate trends between circulation and thermodynamic forcing

https://doi.org/10.1038/s41561-026-02050-w#unit-3-p6

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