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
Book Volume: 49
Journal Issue: 15
DOI: 10.1029/2022GL099692
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.
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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