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Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years
A total of 290 tree-ring samples, collected from six sites in the West Qinling Mountains of China, were used to develop six new standard tree-ring chronologies. In addition, 73 proxy records were assembled in collaboration with Chinese and international scholars, from 27 publically available proxy r...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2013
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3579785/ https://www.ncbi.nlm.nih.gov/pubmed/23451254 http://dx.doi.org/10.1371/journal.pone.0057638 |
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author | Yang, Fengmei Wang, Naiang Shi, Feng Ljungqvist, Fredrik Charpentier Wang, Shigong Fan, Zexin Lu, Junwei |
author_facet | Yang, Fengmei Wang, Naiang Shi, Feng Ljungqvist, Fredrik Charpentier Wang, Shigong Fan, Zexin Lu, Junwei |
author_sort | Yang, Fengmei |
collection | PubMed |
description | A total of 290 tree-ring samples, collected from six sites in the West Qinling Mountains of China, were used to develop six new standard tree-ring chronologies. In addition, 73 proxy records were assembled in collaboration with Chinese and international scholars, from 27 publically available proxy records and 40 tree-ring chronologies that are not available in public datasets. These records were used to reconstruct annual mean temperature variability in the West Qinling Mountains over the past 500 years (AD 1500–1995), using a modified point-by-point regression (hybrid PPR) method. The results demonstrate that the hybrid PPR method successfully integrates the temperature signals from different types of proxies, and that the method preserves a high degree of low-frequency variability. The reconstruction shows greater temperature variability in the West Qinling Mountains than has been found in previous studies. Our temperature reconstruction for this region shows: 1) five distinct cold periods, at approximately AD 1520–1535, AD 1560–1575, AD 1610–1620, AD 1850–1875 and AD 1965–1985, and four warm periods, at approximately AD 1645–1660, AD 1705–1725, AD 1785–1795 and AD 1920–1945; 2) that in this region, the 20(th) century was not the warmest period of the past 500 years; and 3) that a dominant and persistent oscillation of ca. 64 years is significantly identified in the 1640–1790 period. |
format | Online Article Text |
id | pubmed-3579785 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2013 |
publisher | Public Library of Science |
record_format | MEDLINE/PubMed |
spelling | pubmed-35797852013-02-28 Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years Yang, Fengmei Wang, Naiang Shi, Feng Ljungqvist, Fredrik Charpentier Wang, Shigong Fan, Zexin Lu, Junwei PLoS One Research Article A total of 290 tree-ring samples, collected from six sites in the West Qinling Mountains of China, were used to develop six new standard tree-ring chronologies. In addition, 73 proxy records were assembled in collaboration with Chinese and international scholars, from 27 publically available proxy records and 40 tree-ring chronologies that are not available in public datasets. These records were used to reconstruct annual mean temperature variability in the West Qinling Mountains over the past 500 years (AD 1500–1995), using a modified point-by-point regression (hybrid PPR) method. The results demonstrate that the hybrid PPR method successfully integrates the temperature signals from different types of proxies, and that the method preserves a high degree of low-frequency variability. The reconstruction shows greater temperature variability in the West Qinling Mountains than has been found in previous studies. Our temperature reconstruction for this region shows: 1) five distinct cold periods, at approximately AD 1520–1535, AD 1560–1575, AD 1610–1620, AD 1850–1875 and AD 1965–1985, and four warm periods, at approximately AD 1645–1660, AD 1705–1725, AD 1785–1795 and AD 1920–1945; 2) that in this region, the 20(th) century was not the warmest period of the past 500 years; and 3) that a dominant and persistent oscillation of ca. 64 years is significantly identified in the 1640–1790 period. Public Library of Science 2013-02-22 /pmc/articles/PMC3579785/ /pubmed/23451254 http://dx.doi.org/10.1371/journal.pone.0057638 Text en © 2013 Yang et al http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited. |
spellingShingle | Research Article Yang, Fengmei Wang, Naiang Shi, Feng Ljungqvist, Fredrik Charpentier Wang, Shigong Fan, Zexin Lu, Junwei Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title | Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title_full | Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title_fullStr | Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title_full_unstemmed | Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title_short | Multi-Proxy Temperature Reconstruction from the West Qinling Mountains, China, for the Past 500 Years |
title_sort | multi-proxy temperature reconstruction from the west qinling mountains, china, for the past 500 years |
topic | Research Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3579785/ https://www.ncbi.nlm.nih.gov/pubmed/23451254 http://dx.doi.org/10.1371/journal.pone.0057638 |
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