Climate over past millennia

We review evidence for climate change over the past several millennia from instrumental and high-resolution climate "proxy" data sources and climate modeling studies. We focus on changes over the past 1 to 2 millennia. We assess reconstructions and modeling studies analyzing a number of di...

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Published in:Reviews of Geophysics
Main Author: Jones, PD
Format: Article in Journal/Newspaper
Language:unknown
Published: 2004
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/34078/
https://doi.org/10.1029/2003RG000143
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spelling ftuniveastangl:oai:ueaeprints.uea.ac.uk:34078 2023-06-06T11:57:22+02:00 Climate over past millennia Jones, PD 2004 https://ueaeprints.uea.ac.uk/id/eprint/34078/ https://doi.org/10.1029/2003RG000143 unknown Jones, PD (2004) Climate over past millennia. Reviews of Geophysics, 42 (2). ISSN 8755-1209 doi:10.1029/2003RG000143 Article PeerReviewed 2004 ftuniveastangl https://doi.org/10.1029/2003RG000143 2023-04-13T22:31:40Z We review evidence for climate change over the past several millennia from instrumental and high-resolution climate "proxy" data sources and climate modeling studies. We focus on changes over the past 1 to 2 millennia. We assess reconstructions and modeling studies analyzing a number of different climate fields, including atmospheric circulation diagnostics, precipitation, and drought. We devote particular attention to proxy-based reconstructions of temperature patterns in past centuries, which place recent large-scale warming in an appropriate longer-term context. Our assessment affirms the conclusion that late 20th century warmth is unprecedented at hemispheric and, likely, global scales. There is more tentative evidence that particular modes of climate variability, such as the El Niño/Southern Oscillation and the North Atlantic Oscillation, may have exhibited late 20th century behavior that is anomalous in a long-term context. Regional conclusions, particularly for the Southern Hemisphere and parts of the tropics where high-resolution proxy data are sparse, are more circumspect. The dramatic differences between regional and hemispheric/ global past trends, and the distinction between changes in surface temperature and precipitation/drought fields, underscore the limited utility in the use of terms such as the "Little Ice Age" and "Medieval Warm Period" for describing past climate epochs during the last millennium. Comparison of emphirical evidence with proxy-based reconstructions demonstrates that natural factors appaear to explain relatively well the major surface temperature changes of the past millennium through the 9th century (including hemispheric means and some spatial patterns). Only anthropogenic forcing of climate, however, can explain the recent anomalous warming in the late 20th century. Article in Journal/Newspaper North Atlantic North Atlantic oscillation University of East Anglia: UEA Digital Repository Reviews of Geophysics 42 2
institution Open Polar
collection University of East Anglia: UEA Digital Repository
op_collection_id ftuniveastangl
language unknown
description We review evidence for climate change over the past several millennia from instrumental and high-resolution climate "proxy" data sources and climate modeling studies. We focus on changes over the past 1 to 2 millennia. We assess reconstructions and modeling studies analyzing a number of different climate fields, including atmospheric circulation diagnostics, precipitation, and drought. We devote particular attention to proxy-based reconstructions of temperature patterns in past centuries, which place recent large-scale warming in an appropriate longer-term context. Our assessment affirms the conclusion that late 20th century warmth is unprecedented at hemispheric and, likely, global scales. There is more tentative evidence that particular modes of climate variability, such as the El Niño/Southern Oscillation and the North Atlantic Oscillation, may have exhibited late 20th century behavior that is anomalous in a long-term context. Regional conclusions, particularly for the Southern Hemisphere and parts of the tropics where high-resolution proxy data are sparse, are more circumspect. The dramatic differences between regional and hemispheric/ global past trends, and the distinction between changes in surface temperature and precipitation/drought fields, underscore the limited utility in the use of terms such as the "Little Ice Age" and "Medieval Warm Period" for describing past climate epochs during the last millennium. Comparison of emphirical evidence with proxy-based reconstructions demonstrates that natural factors appaear to explain relatively well the major surface temperature changes of the past millennium through the 9th century (including hemispheric means and some spatial patterns). Only anthropogenic forcing of climate, however, can explain the recent anomalous warming in the late 20th century.
format Article in Journal/Newspaper
author Jones, PD
spellingShingle Jones, PD
Climate over past millennia
author_facet Jones, PD
author_sort Jones, PD
title Climate over past millennia
title_short Climate over past millennia
title_full Climate over past millennia
title_fullStr Climate over past millennia
title_full_unstemmed Climate over past millennia
title_sort climate over past millennia
publishDate 2004
url https://ueaeprints.uea.ac.uk/id/eprint/34078/
https://doi.org/10.1029/2003RG000143
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Jones, PD (2004) Climate over past millennia. Reviews of Geophysics, 42 (2). ISSN 8755-1209
doi:10.1029/2003RG000143
op_doi https://doi.org/10.1029/2003RG000143
container_title Reviews of Geophysics
container_volume 42
container_issue 2
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