Claimfe2df9c6f96d9cf547f58deeb0f0e743948984e5632f82b0af69f5a3952ec837·Paper reconstruction — Dunkl, Bastos & Sippel (2026), European summer drying

Claim

For every millimetre of negative circulation-induced soil-moisture anomaly, PD has an additional 0.08 mm of drying relative to NAT, an 8% positive amplification effect.

Evidence (2)

European summer drying largely driven by atmospheric circulation changes since the 1980s — Dynamic warm and dry conditions amplify thermodynamic drying
PD dries on average by an additional 0.08 mm compared to the NAT simulation, resulting in a 8% positive amplification effect.
https://doi.org/10.1038/s41561-026-02050-w#unit-5-p4
European summer drying largely driven by atmospheric circulation changes since the 1980s — Dynamic warm and dry conditions amplify thermodynamic drying
PD dries on average by an additional 0.08 mm compared to the NAT simulation, resulting in a 8% positive amplification effect.
https://doi.org/10.1038/s41561-026-02050-w#unit-5-p4

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