The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360

نویسندگان

چکیده

Recent soil moisture (SM) reconstructions revealed plunging trends and enhanced SM-temperature couplings over the last two decades in dry regions. However, how SM changed whether land-atmosphere interaction was intensified time humid regions remained unknown. Here we reported first six-century-long regional summer reconstruction (1360–2000 CE) western Europe (WE) using three individual tree-ring δ18O chronologies England France. A sharp wet-to-dry change occurred around 1820, earlier than 1850–1900 CE, commonly used historical baseline of anthropogenic climate changes. Enhanced coupling followed, with stronger sea level pressure anomalies years after 1820s. Our results reveal that hotter-drier regime has also become more frequent WE under global warming.

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2022

ISSN: ['1944-8007', '0094-8276']

DOI: https://doi.org/10.1029/2022gl099692