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A less or more dusty future in the Northern Qinghai-Tibetan Plateau?
Dust plays an important role in climate changes as it can alter atmospheric circulation, and global biogeochemical and hydrologic cycling. Many studies have investigated the relationship between dust and temperature in an attempt to predict whether global warming in coming decades to centuries can r...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2014
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4205841/ https://www.ncbi.nlm.nih.gov/pubmed/25335792 http://dx.doi.org/10.1038/srep06672 |
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author | Liu, Xingqi Yu, Zhitong Dong, Hailiang Chen, Huei-Fen |
author_facet | Liu, Xingqi Yu, Zhitong Dong, Hailiang Chen, Huei-Fen |
author_sort | Liu, Xingqi |
collection | PubMed |
description | Dust plays an important role in climate changes as it can alter atmospheric circulation, and global biogeochemical and hydrologic cycling. Many studies have investigated the relationship between dust and temperature in an attempt to predict whether global warming in coming decades to centuries can result in a less or more dusty future. However, dust and temperature changes have rarely been simultaneously reconstructed in the same record. Here we present a 1600-yr-long quantitative record of temperature and dust activity inferred simultaneously from varved Kusai Lake sediments in the northern Qinghai–Tibetan Plateau, NW China. At decadal time scale, our temperature reconstructions are generally in agreement with tree-ring records from Karakorum of Pakistan, and temperature reconstructions of China and North Hemisphere based on compilations of proxy records. A less or more dusty future depends on temperature variations in the Northern Qinghai-Tibetan Plateau, i.e. weak and strong dust activities at centennial time scales are well correlated with low and high June–July–August temperature (average JJA temperature), respectively. This correlation means that stronger summer and winter monsoon should occur at the same times in the northern Qinghai–Tibetan Plateau. |
format | Online Article Text |
id | pubmed-4205841 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2014 |
publisher | Nature Publishing Group |
record_format | MEDLINE/PubMed |
spelling | pubmed-42058412014-10-24 A less or more dusty future in the Northern Qinghai-Tibetan Plateau? Liu, Xingqi Yu, Zhitong Dong, Hailiang Chen, Huei-Fen Sci Rep Article Dust plays an important role in climate changes as it can alter atmospheric circulation, and global biogeochemical and hydrologic cycling. Many studies have investigated the relationship between dust and temperature in an attempt to predict whether global warming in coming decades to centuries can result in a less or more dusty future. However, dust and temperature changes have rarely been simultaneously reconstructed in the same record. Here we present a 1600-yr-long quantitative record of temperature and dust activity inferred simultaneously from varved Kusai Lake sediments in the northern Qinghai–Tibetan Plateau, NW China. At decadal time scale, our temperature reconstructions are generally in agreement with tree-ring records from Karakorum of Pakistan, and temperature reconstructions of China and North Hemisphere based on compilations of proxy records. A less or more dusty future depends on temperature variations in the Northern Qinghai-Tibetan Plateau, i.e. weak and strong dust activities at centennial time scales are well correlated with low and high June–July–August temperature (average JJA temperature), respectively. This correlation means that stronger summer and winter monsoon should occur at the same times in the northern Qinghai–Tibetan Plateau. Nature Publishing Group 2014-10-22 /pmc/articles/PMC4205841/ /pubmed/25335792 http://dx.doi.org/10.1038/srep06672 Text en Copyright © 2014, Macmillan Publishers Limited. All rights reserved http://creativecommons.org/licenses/by-nc-nd/4.0/ This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivs 4.0 International License. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder in order to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/4.0/ |
spellingShingle | Article Liu, Xingqi Yu, Zhitong Dong, Hailiang Chen, Huei-Fen A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title | A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title_full | A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title_fullStr | A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title_full_unstemmed | A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title_short | A less or more dusty future in the Northern Qinghai-Tibetan Plateau? |
title_sort | less or more dusty future in the northern qinghai-tibetan plateau? |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4205841/ https://www.ncbi.nlm.nih.gov/pubmed/25335792 http://dx.doi.org/10.1038/srep06672 |
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