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

Wang L, Liu H, Chen D, Zhang P, Leavitt S, Liu Y, Fang C, Sun C, Cai Q, Gui Z, Liang B, Shi L, Liu F, Zheng Y, Grießinger J (2022)


Publication Type: Journal article

Publication year: 2022

Journal

Book Volume: 49

Journal Issue: 15

DOI: 10.1029/2022GL099692

Abstract

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 and whether the land-atmosphere interaction was intensified over time in humid regions remained unknown. Here we reported the first six-century-long regional summer SM reconstruction (1360-2000 CE) in western Europe (WE) using three individual tree-ring delta O-18 chronologies in England and France. A sharp wet-to-dry change occurred around 1820, earlier than 1850-1900 CE, the commonly used historical baseline of anthropogenic climate changes. Enhanced coupling of SM-temperature followed, with stronger summer sea level pressure anomalies in dry years after the 1820s. Our results reveal that the hotter-drier regime has also become more frequent in humid WE under global warming.

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APA:

Wang, L., Liu, H., Chen, D., Zhang, P., Leavitt, S., Liu, Y.,... Grießinger, J. (2022). The 1820s Marks a Shift to Hotter-Drier Summers in Western Europe Since 1360. Geophysical Research Letters, 49(15). https://doi.org/10.1029/2022GL099692

MLA:

Wang, Lu, et al. "The 1820s Marks a Shift to Hotter-Drier Summers in Western Europe Since 1360." Geophysical Research Letters 49.15 (2022).

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