Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene

Abstract The East Asian winter monsoon (EAWM) is a crucial climate system in Asia, with significant social and economic impacts. Orbital‐scale variability of the EAWM during the Holocene and its associated mechanisms, however, are still not fully understood. Based on a high‐resolution transient simu...

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Published in:Geophysical Research Letters
Main Authors: Peng Zhou, Xinzhou Li, Zhengguo Shi, Yingying Sha, Jing Lei, Zhisheng An
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL105440
https://doaj.org/article/ac97ea1ce78d4a9099ee0064d6624243
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spelling ftdoajarticles:oai:doaj.org/article:ac97ea1ce78d4a9099ee0064d6624243 2024-09-15T18:35:03+00:00 Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene Peng Zhou Xinzhou Li Zhengguo Shi Yingying Sha Jing Lei Zhisheng An 2023-11-01T00:00:00Z https://doi.org/10.1029/2023GL105440 https://doaj.org/article/ac97ea1ce78d4a9099ee0064d6624243 EN eng Wiley https://doi.org/10.1029/2023GL105440 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL105440 https://doaj.org/article/ac97ea1ce78d4a9099ee0064d6624243 Geophysical Research Letters, Vol 50, Iss 21, Pp n/a-n/a (2023) Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL105440 2024-08-05T17:49:23Z Abstract The East Asian winter monsoon (EAWM) is a crucial climate system in Asia, with significant social and economic impacts. Orbital‐scale variability of the EAWM during the Holocene and its associated mechanisms, however, are still not fully understood. Based on a high‐resolution transient simulation by a coupled climate model, we present here a continuous climate evolution of the EAWM in response to orbital forcing. Our simulated springtime EAWM variations, consistent with grain size records of loess, exhibit an obvious strengthening trend since the mid‐Holocene. In winter, a similar increasing trend is also simulated although not statistically significant. Our results suggest that the Holocene EAWM is basically controlled by meridional temperature gradients between high and low latitudes in both seasons. Other than northern insolation forcing, the feedbacks from Arctic sea ice and Eurasian snow cover also modulate the meridional temperature gradients, highlighting their important roles in driving EAWM evolution during the Holocene. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 21
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geophysics. Cosmic physics
QC801-809
spellingShingle Geophysics. Cosmic physics
QC801-809
Peng Zhou
Xinzhou Li
Zhengguo Shi
Yingying Sha
Jing Lei
Zhisheng An
Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
topic_facet Geophysics. Cosmic physics
QC801-809
description Abstract The East Asian winter monsoon (EAWM) is a crucial climate system in Asia, with significant social and economic impacts. Orbital‐scale variability of the EAWM during the Holocene and its associated mechanisms, however, are still not fully understood. Based on a high‐resolution transient simulation by a coupled climate model, we present here a continuous climate evolution of the EAWM in response to orbital forcing. Our simulated springtime EAWM variations, consistent with grain size records of loess, exhibit an obvious strengthening trend since the mid‐Holocene. In winter, a similar increasing trend is also simulated although not statistically significant. Our results suggest that the Holocene EAWM is basically controlled by meridional temperature gradients between high and low latitudes in both seasons. Other than northern insolation forcing, the feedbacks from Arctic sea ice and Eurasian snow cover also modulate the meridional temperature gradients, highlighting their important roles in driving EAWM evolution during the Holocene.
format Article in Journal/Newspaper
author Peng Zhou
Xinzhou Li
Zhengguo Shi
Yingying Sha
Jing Lei
Zhisheng An
author_facet Peng Zhou
Xinzhou Li
Zhengguo Shi
Yingying Sha
Jing Lei
Zhisheng An
author_sort Peng Zhou
title Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
title_short Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
title_full Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
title_fullStr Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
title_full_unstemmed Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene
title_sort strengthened east asian winter monsoon regulated by insolation and arctic sea ice since the middle holocene
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL105440
https://doaj.org/article/ac97ea1ce78d4a9099ee0064d6624243
genre Sea ice
genre_facet Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 21, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL105440
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL105440
https://doaj.org/article/ac97ea1ce78d4a9099ee0064d6624243
op_doi https://doi.org/10.1029/2023GL105440
container_title Geophysical Research Letters
container_volume 50
container_issue 21
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