The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records
Asian summer monsoon (ASM) variability significantly affects hydro-climate, and thus socio-economics, in the East Asian region, where nearly one-third of the global population resides. Over the last two decades, speleothem δ 18 O records from China have been utilized to reconstruct ASM variability a...
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ftdoajarticles:oai:doaj.org/article:b16445daa3c74f399a48dba10a12ab6e 2023-05-15T17:34:10+02:00 The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records Haiwei Zhang Yassine Ait Brahim Hanying Li Jingyao Zhao Gayatri Kathayat Ye Tian Jonathan Baker Jian Wang Fan Zhang Youfeng Ning R. Lawrence Edwards Hai Cheng 2019-07-01T00:00:00Z https://doi.org/10.3390/quat2030026 https://doaj.org/article/b16445daa3c74f399a48dba10a12ab6e EN eng MDPI AG https://www.mdpi.com/2571-550X/2/3/26 https://doaj.org/toc/2571-550X 2571-550X doi:10.3390/quat2030026 https://doaj.org/article/b16445daa3c74f399a48dba10a12ab6e Quaternary, Vol 2, Iss 3, p 26 (2019) ASM SISAL speleothem oxygen isotope paleoclimate China Human evolution GN281-289 Stratigraphy QE640-699 article 2019 ftdoajarticles https://doi.org/10.3390/quat2030026 2022-12-31T12:31:40Z Asian summer monsoon (ASM) variability significantly affects hydro-climate, and thus socio-economics, in the East Asian region, where nearly one-third of the global population resides. Over the last two decades, speleothem δ 18 O records from China have been utilized to reconstruct ASM variability and its underlying forcing mechanisms on orbital to seasonal timescales. Here, we use the Speleothem Isotopes Synthesis and Analysis database (SISAL_v1) to present an overview of hydro-climate variability related to the ASM during three periods: the late Pleistocene, the Holocene, and the last two millennia. We highlight the possible global teleconnections and forcing mechanisms of the ASM on different timescales. The longest composite stalagmite δ 18 O record over the past 640 kyr BP from the region demonstrates that ASM variability on orbital timescales is dominated by the 23 kyr precessional cycles, which are in phase with Northern Hemisphere summer insolation (NHSI). During the last glacial, millennial changes in the intensity of the ASM appear to be controlled by North Atlantic climate and oceanic feedbacks. During the Holocene, changes in ASM intensity were primarily controlled by NHSI. However, the spatio-temporal distribution of monsoon rain belts may vary with changes in ASM intensity on decadal to millennial timescales. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Quaternary 2 3 26 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
ASM SISAL speleothem oxygen isotope paleoclimate China Human evolution GN281-289 Stratigraphy QE640-699 |
spellingShingle |
ASM SISAL speleothem oxygen isotope paleoclimate China Human evolution GN281-289 Stratigraphy QE640-699 Haiwei Zhang Yassine Ait Brahim Hanying Li Jingyao Zhao Gayatri Kathayat Ye Tian Jonathan Baker Jian Wang Fan Zhang Youfeng Ning R. Lawrence Edwards Hai Cheng The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
topic_facet |
ASM SISAL speleothem oxygen isotope paleoclimate China Human evolution GN281-289 Stratigraphy QE640-699 |
description |
Asian summer monsoon (ASM) variability significantly affects hydro-climate, and thus socio-economics, in the East Asian region, where nearly one-third of the global population resides. Over the last two decades, speleothem δ 18 O records from China have been utilized to reconstruct ASM variability and its underlying forcing mechanisms on orbital to seasonal timescales. Here, we use the Speleothem Isotopes Synthesis and Analysis database (SISAL_v1) to present an overview of hydro-climate variability related to the ASM during three periods: the late Pleistocene, the Holocene, and the last two millennia. We highlight the possible global teleconnections and forcing mechanisms of the ASM on different timescales. The longest composite stalagmite δ 18 O record over the past 640 kyr BP from the region demonstrates that ASM variability on orbital timescales is dominated by the 23 kyr precessional cycles, which are in phase with Northern Hemisphere summer insolation (NHSI). During the last glacial, millennial changes in the intensity of the ASM appear to be controlled by North Atlantic climate and oceanic feedbacks. During the Holocene, changes in ASM intensity were primarily controlled by NHSI. However, the spatio-temporal distribution of monsoon rain belts may vary with changes in ASM intensity on decadal to millennial timescales. |
format |
Article in Journal/Newspaper |
author |
Haiwei Zhang Yassine Ait Brahim Hanying Li Jingyao Zhao Gayatri Kathayat Ye Tian Jonathan Baker Jian Wang Fan Zhang Youfeng Ning R. Lawrence Edwards Hai Cheng |
author_facet |
Haiwei Zhang Yassine Ait Brahim Hanying Li Jingyao Zhao Gayatri Kathayat Ye Tian Jonathan Baker Jian Wang Fan Zhang Youfeng Ning R. Lawrence Edwards Hai Cheng |
author_sort |
Haiwei Zhang |
title |
The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
title_short |
The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
title_full |
The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
title_fullStr |
The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
title_full_unstemmed |
The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ 18 O Records |
title_sort |
asian summer monsoon: teleconnections and forcing mechanisms—a review from chinese speleothem δ 18 o records |
publisher |
MDPI AG |
publishDate |
2019 |
url |
https://doi.org/10.3390/quat2030026 https://doaj.org/article/b16445daa3c74f399a48dba10a12ab6e |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Quaternary, Vol 2, Iss 3, p 26 (2019) |
op_relation |
https://www.mdpi.com/2571-550X/2/3/26 https://doaj.org/toc/2571-550X 2571-550X doi:10.3390/quat2030026 https://doaj.org/article/b16445daa3c74f399a48dba10a12ab6e |
op_doi |
https://doi.org/10.3390/quat2030026 |
container_title |
Quaternary |
container_volume |
2 |
container_issue |
3 |
container_start_page |
26 |
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1766132918961307648 |