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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