The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies

ABSTRACTAccurate reconstructed series are crucial for studying the differences in regional hydroclimatic variations in Europe over the past millennium. Using hierarchical clustering analysis and stepwise regression methods, we reconstructed yearly time series of the summer standardized precipitation...

Full description

Bibliographic Details
Main Authors: Liang Zhang, Yang Liu, Jingyun Zheng, Zhixin Hao
Format: Article
Language:English
Published: Taylor & Francis Group 2023-08-01
Series:Big Earth Data
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/20964471.2023.2247864
_version_ 1797731330396520448
author Liang Zhang
Yang Liu
Jingyun Zheng
Zhixin Hao
author_facet Liang Zhang
Yang Liu
Jingyun Zheng
Zhixin Hao
author_sort Liang Zhang
collection DOAJ
description ABSTRACTAccurate reconstructed series are crucial for studying the differences in regional hydroclimatic variations in Europe over the past millennium. Using hierarchical clustering analysis and stepwise regression methods, we reconstructed yearly time series of the summer standardized precipitation evapotranspiration index (SPEI) for six European regions over the past millennium. Our analysis also revealed prominent regional hydroclimatic differences in multidecadal signals over the past 500 years. For instance, in the 1500s–1570s (from the beginning of the 1500s to the end of the 1570s), drying trends were observed in northern and southeastern Europe, whereas southwestern Europe experienced a wetting trend. Moreover, drying trends were observed in northern and central Europe in the 1640s–1670s. Additionally, wetting trends were observed in western and central Europe during the 1830s–1850s, with drying trends in northern and southeastern Europe. Notably, the hydroclimatic variations in most European regions showed drying trends in the 1920s–1950s, especially in southern Europe. By utilizing large amounts of tree-ring samples and directly comparing regional hydroclimatic variations, our reconstructions provide a consistent and comprehensive dataset for further analysis. The reconstructed dataset is available at https://doi.org/10.57760/sciencedb.07215.
first_indexed 2024-03-12T11:57:13Z
format Article
id doaj.art-f1d868ca14354040b4bf29d5e115195a
institution Directory Open Access Journal
issn 2096-4471
2574-5417
language English
last_indexed 2024-03-12T11:57:13Z
publishDate 2023-08-01
publisher Taylor & Francis Group
record_format Article
series Big Earth Data
spelling doaj.art-f1d868ca14354040b4bf29d5e115195a2023-08-30T17:30:05ZengTaylor & Francis GroupBig Earth Data2096-44712574-54172023-08-0112310.1080/20964471.2023.2247864The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologiesLiang Zhang0Yang Liu1Jingyun Zheng2Zhixin Hao3Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, ChinaKey Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, ChinaKey Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, ChinaKey Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, ChinaABSTRACTAccurate reconstructed series are crucial for studying the differences in regional hydroclimatic variations in Europe over the past millennium. Using hierarchical clustering analysis and stepwise regression methods, we reconstructed yearly time series of the summer standardized precipitation evapotranspiration index (SPEI) for six European regions over the past millennium. Our analysis also revealed prominent regional hydroclimatic differences in multidecadal signals over the past 500 years. For instance, in the 1500s–1570s (from the beginning of the 1500s to the end of the 1570s), drying trends were observed in northern and southeastern Europe, whereas southwestern Europe experienced a wetting trend. Moreover, drying trends were observed in northern and central Europe in the 1640s–1670s. Additionally, wetting trends were observed in western and central Europe during the 1830s–1850s, with drying trends in northern and southeastern Europe. Notably, the hydroclimatic variations in most European regions showed drying trends in the 1920s–1950s, especially in southern Europe. By utilizing large amounts of tree-ring samples and directly comparing regional hydroclimatic variations, our reconstructions provide a consistent and comprehensive dataset for further analysis. The reconstructed dataset is available at https://doi.org/10.57760/sciencedb.07215.https://www.tandfonline.com/doi/10.1080/20964471.2023.2247864Europehydroclimatic variationsregional reconstructiontree-ring chronologiespast millennium
spellingShingle Liang Zhang
Yang Liu
Jingyun Zheng
Zhixin Hao
The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
Big Earth Data
Europe
hydroclimatic variations
regional reconstruction
tree-ring chronologies
past millennium
title The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
title_full The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
title_fullStr The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
title_full_unstemmed The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
title_short The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies
title_sort summer standardized precipitation evapotranspiration index spei dataset for six european regions over the past millennium reconstructed by tree ring chronologies
topic Europe
hydroclimatic variations
regional reconstruction
tree-ring chronologies
past millennium
url https://www.tandfonline.com/doi/10.1080/20964471.2023.2247864
work_keys_str_mv AT liangzhang thesummerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT yangliu thesummerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT jingyunzheng thesummerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT zhixinhao thesummerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT liangzhang summerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT yangliu summerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT jingyunzheng summerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies
AT zhixinhao summerstandardizedprecipitationevapotranspirationindexspeidatasetforsixeuropeanregionsoverthepastmillenniumreconstructedbytreeringchronologies