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

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 reporte...

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Main Authors: Lu Wang, Hongyan Liu, Deliang Chen, Peng Zhang, Steven Leavitt, Yu Liu, Congxi Fang, Changfeng Sun, Qiufang Cai, Zhengyang Gui, Boyi Liang, Liang Shi, Feng Liu, Yukun Zheng, Jussi Grießinger
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Language:English
Published: Wiley 2022-08-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1029/2022GL099692
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author Lu Wang
Hongyan Liu
Deliang Chen
Peng Zhang
Steven Leavitt
Yu Liu
Congxi Fang
Changfeng Sun
Qiufang Cai
Zhengyang Gui
Boyi Liang
Liang Shi
Feng Liu
Yukun Zheng
Jussi Grießinger
author_facet Lu Wang
Hongyan Liu
Deliang Chen
Peng Zhang
Steven Leavitt
Yu Liu
Congxi Fang
Changfeng Sun
Qiufang Cai
Zhengyang Gui
Boyi Liang
Liang Shi
Feng Liu
Yukun Zheng
Jussi Grießinger
author_sort Lu Wang
collection DOAJ
description 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 δ18O 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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institution OA Journals
issn 0094-8276
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language English
publishDate 2022-08-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-54072ccd088540dbacdce57bb646cd2e2025-08-20T02:11:38ZengWileyGeophysical Research Letters0094-82761944-80072022-08-014915n/an/a10.1029/2022GL099692The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360Lu Wang0Hongyan Liu1Deliang Chen2Peng Zhang3Steven Leavitt4Yu Liu5Congxi Fang6Changfeng Sun7Qiufang Cai8Zhengyang Gui9Boyi Liang10Liang Shi11Feng Liu12Yukun Zheng13Jussi Grießinger14College of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaCollege of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaDepartment of Earth Sciences University of Gothenburg Gothenburg SwedenDepartment of Earth Sciences University of Gothenburg Gothenburg SwedenLaboratory of Tree‐Ring Research University of Arizona Tucson AZ USAThe State Key Laboratory of Loess and Quaternary Geology Institute of Earth Environment Chinese Academy of Sciences Xi'an ChinaThe State Key Laboratory of Loess and Quaternary Geology Institute of Earth Environment Chinese Academy of Sciences Xi'an ChinaInstitute of Global Environmental Change Xi'an Jiaotong University Xi'an ChinaThe State Key Laboratory of Loess and Quaternary Geology Institute of Earth Environment Chinese Academy of Sciences Xi'an ChinaCollege of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaCollege of Forestry Precision Forestry Key Laboratory of Beijing Beijing Forestry University Beijing ChinaCollege of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaCollege of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaCollege of Urban and Environmental Sciences, Sino‐French Institute of Earth System Science Peking University Beijing ChinaFriedrich‐Alexander‐University Erlangen‐Nürnberg Institute of Geography Wetterkreuz GermanyAbstract 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 δ18O 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.https://doi.org/10.1029/2022GL099692soil moistureland‐atmosphere couplingclimate changetree‐ring isotopewestern Europe
spellingShingle Lu Wang
Hongyan Liu
Deliang Chen
Peng Zhang
Steven Leavitt
Yu Liu
Congxi Fang
Changfeng Sun
Qiufang Cai
Zhengyang Gui
Boyi Liang
Liang Shi
Feng Liu
Yukun Zheng
Jussi Grießinger
The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
Geophysical Research Letters
soil moisture
land‐atmosphere coupling
climate change
tree‐ring isotope
western Europe
title The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
title_full The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
title_fullStr The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
title_full_unstemmed The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
title_short The 1820s Marks a Shift to Hotter‐Drier Summers in Western Europe Since 1360
title_sort 1820s marks a shift to hotter drier summers in western europe since 1360
topic soil moisture
land‐atmosphere coupling
climate change
tree‐ring isotope
western Europe
url https://doi.org/10.1029/2022GL099692
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