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  "retrievedAt": "2026-08-24T19:49:57.955Z",
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    "text": "Changes in the occurrence of summer weather regimes are associated with the regional dynamic temperature, soil-moisture, and VPD patterns, providing a circulation mechanism for heterogeneous drying."
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      "text": "Three of five identified summer weather regimes have significant frequency trends: declining cyclonic Northern European conditions (WR1), declining Atlantic-anticyclonic/southeastern-European-cyclonic conditions (WR2), and increasing Mediterranean/Central European anticyclonic conditions (WR3). Their occurrence changes are associated with regional dynamic hydroclimate trends.",
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      "text": "Three of five k-means-identified summertime weather regimes have statistically significant occurrence trends since 1980: cyclonic Northern European conditions (WR1) and the Atlantic-anticyclonic/southeastern-European-cyclonic bipolar pattern (WR2) decrease, while Mediterranean and Central European anticyclonic conditions (WR3) increase.",
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      "text": "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.",
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