Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans
Variations of precipitation, also called the Meiyu rain, in the East Asian summer monsoon (EASM) domain during the last millennium could help enlighten the hydrological response to future global warming. Here we present a precisely dated and highly resolved stalagmite δ18O record from the Yongxing C...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:fe980698ffbe4ecba6ab5804f91ae026 2023-05-15T17:28:52+02:00 Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans F. Duan Z. Zhang Y. Wang J. Chen Z. Liao S. Chen Q. Shao K. Zhao 2020-03-01 https://doi.org/10.5194/cp-16-475-2020 https://www.clim-past.net/16/475/2020/cp-16-475-2020.pdf https://doaj.org/article/fe980698ffbe4ecba6ab5804f91ae026 en eng Copernicus Publications doi:10.5194/cp-16-475-2020 1814-9324 1814-9332 https://www.clim-past.net/16/475/2020/cp-16-475-2020.pdf https://doaj.org/article/fe980698ffbe4ecba6ab5804f91ae026 undefined Climate of the Past, Vol 16, Pp 475-485 (2020) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2020 fttriple https://doi.org/10.5194/cp-16-475-2020 2023-01-22T19:26:17Z Variations of precipitation, also called the Meiyu rain, in the East Asian summer monsoon (EASM) domain during the last millennium could help enlighten the hydrological response to future global warming. Here we present a precisely dated and highly resolved stalagmite δ18O record from the Yongxing Cave, central China. Our new record, combined with a previously published one from the same cave, indicates that the Meiyu rain has changed dramatically in association with the global temperature change. In particular, our record shows that the Meiyu rain was weakened during the Medieval Climate Anomaly (MCA) but intensified during the Little Ice Age (LIA). During the Current Warm Period (CWP), our record indicates a similar weakening of the Meiyu rain. Furthermore, during the MCA and CWP, our records show that the atmospheric precipitation is similarly wet in northern China and similarly dry in central China, but relatively wet during the CWP in southern China. This spatial discrepancy indicates a complicated localized response of the regional precipitation to the anthropogenic forcing. The weakened (intensified) Meiyu rain during the MCA (LIA) matches well with the warm (cold) phases of Northern Hemisphere surface air temperature. This Meiyu rain pattern also corresponds well to the climatic conditions over the tropical Indo-Pacific warm pool. On the other hand, our record shows a strong association with the North Atlantic climate as well. The reduced (increased) Meiyu rain correlates well with positive (negative) phases of the North Atlantic Oscillation. In addition, our record links well to the strong (weak) Atlantic meridional overturning circulation during the MCA (LIA) period. All abovementioned localized correspondences and remote teleconnections on decadal to centennial timescales indicate that the Meiyu rain was coupled closely with oceanic processes in the tropical Pacific and North Atlantic oceans during the MCA and LIA. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Unknown Pacific Climate of the Past 16 2 475 485 |
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English |
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envir geo F. Duan Z. Zhang Y. Wang J. Chen Z. Liao S. Chen Q. Shao K. Zhao Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
topic_facet |
envir geo |
description |
Variations of precipitation, also called the Meiyu rain, in the East Asian summer monsoon (EASM) domain during the last millennium could help enlighten the hydrological response to future global warming. Here we present a precisely dated and highly resolved stalagmite δ18O record from the Yongxing Cave, central China. Our new record, combined with a previously published one from the same cave, indicates that the Meiyu rain has changed dramatically in association with the global temperature change. In particular, our record shows that the Meiyu rain was weakened during the Medieval Climate Anomaly (MCA) but intensified during the Little Ice Age (LIA). During the Current Warm Period (CWP), our record indicates a similar weakening of the Meiyu rain. Furthermore, during the MCA and CWP, our records show that the atmospheric precipitation is similarly wet in northern China and similarly dry in central China, but relatively wet during the CWP in southern China. This spatial discrepancy indicates a complicated localized response of the regional precipitation to the anthropogenic forcing. The weakened (intensified) Meiyu rain during the MCA (LIA) matches well with the warm (cold) phases of Northern Hemisphere surface air temperature. This Meiyu rain pattern also corresponds well to the climatic conditions over the tropical Indo-Pacific warm pool. On the other hand, our record shows a strong association with the North Atlantic climate as well. The reduced (increased) Meiyu rain correlates well with positive (negative) phases of the North Atlantic Oscillation. In addition, our record links well to the strong (weak) Atlantic meridional overturning circulation during the MCA (LIA) period. All abovementioned localized correspondences and remote teleconnections on decadal to centennial timescales indicate that the Meiyu rain was coupled closely with oceanic processes in the tropical Pacific and North Atlantic oceans during the MCA and LIA. |
format |
Article in Journal/Newspaper |
author |
F. Duan Z. Zhang Y. Wang J. Chen Z. Liao S. Chen Q. Shao K. Zhao |
author_facet |
F. Duan Z. Zhang Y. Wang J. Chen Z. Liao S. Chen Q. Shao K. Zhao |
author_sort |
F. Duan |
title |
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
title_short |
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
title_full |
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
title_fullStr |
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
title_full_unstemmed |
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans |
title_sort |
hydrological variations in central china over the past millennium and their links to the tropical pacific and north atlantic oceans |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/cp-16-475-2020 https://www.clim-past.net/16/475/2020/cp-16-475-2020.pdf https://doaj.org/article/fe980698ffbe4ecba6ab5804f91ae026 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
Climate of the Past, Vol 16, Pp 475-485 (2020) |
op_relation |
doi:10.5194/cp-16-475-2020 1814-9324 1814-9332 https://www.clim-past.net/16/475/2020/cp-16-475-2020.pdf https://doaj.org/article/fe980698ffbe4ecba6ab5804f91ae026 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/cp-16-475-2020 |
container_title |
Climate of the Past |
container_volume |
16 |
container_issue |
2 |
container_start_page |
475 |
op_container_end_page |
485 |
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1766121990034292736 |