Grand dipole response of Asian summer monsoon to orbital forcing

The coherent continental-wide speleothem water isotope records are accompanied by regionally inconsistent moisture patterns within the Asian summer monsoon (ASM) region, leaving a disputed explanation of monsoonal hydroclimate variability at the orbital timescale. Here, the transient simulation forced by orbital parameters during the past 300,000 years in an isotope-enabled fully coupled model shows that the complex ASM response can be understood as a grand dipole pattern of oxygen isotope and rainfall between South Asia and Japan, with South China lying in a hybrid transition region. While the dipole monsoon rainfall change between South Asia and Japan is related to the large-scale circulation adjustment in response to Northern Hemisphere summer insolation, the dipole oxygen isotope pattern is associated with the changing contribution of moisture sources. Our results provide new clues to reconcile ASM hydroclimate patterns at orbital timescale as revealed by the water isotope records and other hydrological proxies.

Authors

Institutions

Publication Details

Journal
npj Climate and Atmospheric Science
Published
2024-08-30
DOI
https://doi.org/10.1038/s41612-024-00749-4
Citations
18
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
6.77

Funders

Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Grand dipole response of Asian summer monsoon to orbital forcing

Mi Yan, Jian Liu, Steven C. Clemens, Zhaowei Jing et al.
18 citations
npj Climate and Atmospheric Science
Geology and Paleoclimatology Research
6.77
article

Grand dipole response of Asian summer monsoon to orbital forcing

Mi Yan, Jian Liu, Steven C. Clemens, Zhaowei Jing, Qin Wen, Liang Ning, Zhengyu Liu, Yongjin Wang
article en
18 citations

Abstract

The coherent continental-wide speleothem water isotope records are accompanied by regionally inconsistent moisture patterns within the Asian summer monsoon (ASM) region, leaving a disputed explanation of monsoonal hydroclimate variability at the orbital timescale. Here, the transient simulation forced by orbital parameters during the past 300,000 years in an isotope-enabled fully coupled model shows that the complex ASM response can be understood as a grand dipole pattern of oxygen isotope and rainfall between South Asia and Japan, with South China lying in a hybrid transition region. While the dipole monsoon rainfall change between South Asia and Japan is related to the large-scale circulation adjustment in response to Northern Hemisphere summer insolation, the dipole oxygen isotope pattern is associated with the changing contribution of moisture sources. Our results provide new clues to reconcile ASM hydroclimate patterns at orbital timescale as revealed by the water isotope records and other hydrological proxies.

npj Climate and Atmospheric ScienceVol. 7(1)
Nanjing Normal University (CN), Brown University (US), Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application (CN), Laoshan Laboratory, The Ohio State University (US)
National Science Foundation, Priority Academic Program Development of Jiangsu Higher Education Institutions, National Key Research and Development Program of China, State Key Laboratory of Loess and Quaternary Geology
Climate action
Openalex Percentile: Top 2%
Geology and Paleoclimatology Research
6.77
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.