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DOI10.1007/s00382-024-07166-6
Enhancing spatiotemporal paleoclimate reconstructions of hydroclimate across the Mediterranean over the last millennium
发表日期2024
ISSN0930-7575
EISSN1432-0894
英文摘要The Mediterranean region is projected to experience severe drying trends and more extreme hydroclimate events as a consequence of anthropogenic climate change over the next century. In some places this signal may have already emerged from natural variability, but uncertainty in long-term paleoclimate reconstructions can be a significant challenge to the detection of the influence of rising CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$\text {CO}_{2}$$\end{document} on droughts. Here we provide expanded context for recent and future hydroclimate changes with a new high-resolution (0.5o\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$<^>o$$\end{document}) spatial reconstruction of the Palmer Drought Severity Index (PDSI) using a tree-ring network that spans much of the last millennium. This network provides new perspective on the existing Old World Drought Atlas (OWDA) and allows us to characterize differences between OWDA and our reconstruction. In light of the uncertainties we identify, we also reexamine previous conclusions about the severity of recent droughts in the context of earlier centuries. We find that, in both the western Mediterranean and the Levant, recent dry periods remain the worst in at least the last 500 years, but our assessment of the significance and confidence in this finding is affected by differences in the tree-ring networks used for the reconstructions. Long millennium-length hydroclimate reconstructions in the Mediterranean do provide the opportunity to understand variability and trends in the hydroclimate of the region, but extant uncertainties arising from the existing tree-ring chronology network and methodological choices call attention to locations that require further proxy collection, chronology updates, and statistical scrutiny.
英文关键词Drought; Megadrought; Dendrochronology; Uncertainty; Hydroclimate; Mediterranean
语种英语
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:001194788800001
来源期刊CLIMATE DYNAMICS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/290191
作者单位University of Arizona; University of Arizona; University of Batna; Universite Mouloud Mammeri de Tizi Ouzou; Kastamonu University; Lebanese University; University Balamand; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Pirenaico de Ecologia (IPE); Universidad Pablo de Olavide; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Institut de Recherche pour le Developpement (IRD); Avignon Universite; University of Turin; National Oceanic Atmospheric Admin (NOAA) - USA; National Geodetic Survey, NOAA; National Aeronautics & Space Administration (NASA); NASA Goddard Space Flight Center; Goddard Institute for Space Studies; Stefan cel Mare University of Suceava
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GB/T 7714
. Enhancing spatiotemporal paleoclimate reconstructions of hydroclimate across the Mediterranean over the last millennium[J],2024.
APA (2024).Enhancing spatiotemporal paleoclimate reconstructions of hydroclimate across the Mediterranean over the last millennium.CLIMATE DYNAMICS.
MLA "Enhancing spatiotemporal paleoclimate reconstructions of hydroclimate across the Mediterranean over the last millennium".CLIMATE DYNAMICS (2024).
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