Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years

Understanding the past significant changes of the East Asia Summer Monsoon (EASM) and Winter Monsoon (EAWM) is critical for improving the projections of future climate over East Asia. One key issue that has remained outstanding from the paleo-climatic records is whether the evolution of the EASM and...

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Published in:Nature Communications
Main Authors: Wen, Xinyu, Liu, Zhengyu, Wang, Shaowu, Cheng, Jun, Zhu, Jiang
Other Authors: Wen, XY (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China.; Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China., Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China., Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China., Univ Wisconsin, Dept Atmospher & Ocean Sci, Nelson Inst Environm Studies, Madison, WI 53706 USA., Univ Wisconsin, Ctr Climat Res, Nelson Inst Environm Studies, Madison, WI 53706 USA., Nanjing Univ Informat Sci & Technol, Polar Climate Syst & Global Change Lab, Nanjing 210044, Jiangsu, Peoples R China., Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: NATURE COMMUNICATIONS 2016
Subjects:
SOUTHERN-HEMISPHERE
HIGH-RESOLUTION
GLOBAL MONSOON
CLIMATE
DEGLACIATION
RECORD
CCSM3
MODEL
VARIABILITY
SIMULATION
North Atlantic
Online Access:https://hdl.handle.net/20.500.11897/433241
https://doi.org/10.1038/ncomms11999
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spelling ftpekinguniv:oai:localhost:20.500.11897/433241 2023-05-15T17:33:14+02:00 Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years Wen, Xinyu Liu, Zhengyu Wang, Shaowu Cheng, Jun Zhu, Jiang Wen, XY (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China.; Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China. Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China. Univ Wisconsin, Dept Atmospher & Ocean Sci, Nelson Inst Environm Studies, Madison, WI 53706 USA. Univ Wisconsin, Ctr Climat Res, Nelson Inst Environm Studies, Madison, WI 53706 USA. Nanjing Univ Informat Sci & Technol, Polar Climate Syst & Global Change Lab, Nanjing 210044, Jiangsu, Peoples R China. Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China. 2016 https://hdl.handle.net/20.500.11897/433241 https://doi.org/10.1038/ncomms11999 en eng NATURE COMMUNICATIONS NATURE COMMUNICATIONS.2016,7. 1389070 2041-1723 http://hdl.handle.net/20.500.11897/433241 doi:10.1038/ncomms11999 27328616 WOS:000379090200001 PubMed SCI SOUTHERN-HEMISPHERE HIGH-RESOLUTION GLOBAL MONSOON CLIMATE DEGLACIATION RECORD CCSM3 MODEL VARIABILITY SIMULATION Journal 2016 ftpekinguniv https://doi.org/20.500.11897/433241 https://doi.org/10.1038/ncomms11999 2021-08-01T10:46:44Z Understanding the past significant changes of the East Asia Summer Monsoon (EASM) and Winter Monsoon (EAWM) is critical for improving the projections of future climate over East Asia. One key issue that has remained outstanding from the paleo-climatic records is whether the evolution of the EASM and EAWM are correlated. Here, using a set of long-term transient simulations of the climate evolution of the last 21,000 years, we show that the EASM and EAWM are positively correlated on the orbital timescale in response to the precessional forcing, but are anti-correlated on millennial timescales in response to North Atlantic melt water forcing. The relation between EASM and EAWM can differ dramatically for different timescales because of the different response mechanisms, highlighting the complex dynamics of the East Asian monsoon system and the challenges for future projection. National Science Foundation of China [41130105, 41130962, 41005035, 41206024]; US NSF; Office of Science (BER), DOE SCI(E) PubMed ARTICLE xwen@pku.edu.cn 11999 7 Journal/Newspaper North Atlantic Peking University Institutional Repository (PKU IR) Nature Communications 7 1
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language English
topic SOUTHERN-HEMISPHERE
HIGH-RESOLUTION
GLOBAL MONSOON
CLIMATE
DEGLACIATION
RECORD
CCSM3
MODEL
VARIABILITY
SIMULATION
spellingShingle SOUTHERN-HEMISPHERE
HIGH-RESOLUTION
GLOBAL MONSOON
CLIMATE
DEGLACIATION
RECORD
CCSM3
MODEL
VARIABILITY
SIMULATION
Wen, Xinyu
Liu, Zhengyu
Wang, Shaowu
Cheng, Jun
Zhu, Jiang
Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
topic_facet SOUTHERN-HEMISPHERE
HIGH-RESOLUTION
GLOBAL MONSOON
CLIMATE
DEGLACIATION
RECORD
CCSM3
MODEL
VARIABILITY
SIMULATION
description Understanding the past significant changes of the East Asia Summer Monsoon (EASM) and Winter Monsoon (EAWM) is critical for improving the projections of future climate over East Asia. One key issue that has remained outstanding from the paleo-climatic records is whether the evolution of the EASM and EAWM are correlated. Here, using a set of long-term transient simulations of the climate evolution of the last 21,000 years, we show that the EASM and EAWM are positively correlated on the orbital timescale in response to the precessional forcing, but are anti-correlated on millennial timescales in response to North Atlantic melt water forcing. The relation between EASM and EAWM can differ dramatically for different timescales because of the different response mechanisms, highlighting the complex dynamics of the East Asian monsoon system and the challenges for future projection. National Science Foundation of China [41130105, 41130962, 41005035, 41206024]; US NSF; Office of Science (BER), DOE SCI(E) PubMed ARTICLE xwen@pku.edu.cn 11999 7
author2 Wen, XY (reprint author), Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China.; Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China.
Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China.
Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China.
Univ Wisconsin, Dept Atmospher & Ocean Sci, Nelson Inst Environm Studies, Madison, WI 53706 USA.
Univ Wisconsin, Ctr Climat Res, Nelson Inst Environm Studies, Madison, WI 53706 USA.
Nanjing Univ Informat Sci & Technol, Polar Climate Syst & Global Change Lab, Nanjing 210044, Jiangsu, Peoples R China.
Wen, XY (reprint author), Peking Univ, Sch Phys, Lab Climate & Ocean Atmosphere Studies, Beijing 100871, Peoples R China.
format Journal/Newspaper
author Wen, Xinyu
Liu, Zhengyu
Wang, Shaowu
Cheng, Jun
Zhu, Jiang
author_facet Wen, Xinyu
Liu, Zhengyu
Wang, Shaowu
Cheng, Jun
Zhu, Jiang
author_sort Wen, Xinyu
title Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
title_short Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
title_full Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
title_fullStr Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
title_full_unstemmed Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years
title_sort correlation and anti-correlation of the east asian summer and winter monsoons during the last 21,000 years
publisher NATURE COMMUNICATIONS
publishDate 2016
url https://hdl.handle.net/20.500.11897/433241
https://doi.org/10.1038/ncomms11999
genre North Atlantic
genre_facet North Atlantic
op_source PubMed
SCI
op_relation NATURE COMMUNICATIONS.2016,7.
1389070
2041-1723
http://hdl.handle.net/20.500.11897/433241
doi:10.1038/ncomms11999
27328616
WOS:000379090200001
op_doi https://doi.org/20.500.11897/433241
https://doi.org/10.1038/ncomms11999
container_title Nature Communications
container_volume 7
container_issue 1
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