For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for 55% of continental soil-moisture drying, with particularly large regional shares.

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For 1980–2024, circulation-induced dynamics account for 45% of summer warming, dominate the European precipitation decline, and account for 55% of continental soil-moisture drying, with particularly ltested-undermined

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