Thresholds in East Asian marginal seas circulation due to deglacial sea level rise

East Asian marginal seas (EAMS) circulation is closely configurated by sea level rise during the last deglaciation. Here, we perform simulations to reconstruct the EAMS circulation on the basis of sea levels from −90 to 0 m of the present, using a high-resolution regional ocean circulation model under present-day fixed surface and lateral boundary conditions. Our results show that the EAMS circulation underwent twice abrupt changes: a rapid initiation of its modern structure when sea level rise exceeded −40 m, followed by a temporary overshoot of the Japan-Sea throughflows at −5 m. These nonlinear processes are caused by the opening of the Soya Strait and thus formation of the modern EAMS-circulation structure, and a transient absence of the circulation resembling a Kuroshio Large Meander following around-island integral constraint, respectively. Conceptually, our findings introduce the around-island integral constraint on abrupt shift in the global marginal-sea circulation during the last deglaciation.

Authors

Institutions

Publication Details

Journal
npj Climate and Atmospheric Science
Published
2025-03-01
DOI
https://doi.org/10.1038/s41612-025-00927-y
Citations
1
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
1.79
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Thresholds in East Asian marginal seas circulation due to deglacial sea level rise

Xun Gong, Dong Zhi, Lester Lembke‐Jene, Gerrit Lohmann et al.
1 citations
npj Climate and Atmospheric Science
Geophysics and Gravity Measurements
1.79
article

Thresholds in East Asian marginal seas circulation due to deglacial sea level rise

Xun Gong, Dong Zhi, Lester Lembke‐Jene, Gerrit Lohmann, Xiaopei Lin, Yang Yu, Xuesong Wang, Guangliang Liu, Jiayu Zheng, Xuefa Shi
article en
1 citations

Abstract

East Asian marginal seas (EAMS) circulation is closely configurated by sea level rise during the last deglaciation. Here, we perform simulations to reconstruct the EAMS circulation on the basis of sea levels from −90 to 0 m of the present, using a high-resolution regional ocean circulation model under present-day fixed surface and lateral boundary conditions. Our results show that the EAMS circulation underwent twice abrupt changes: a rapid initiation of its modern structure when sea level rise exceeded −40 m, followed by a temporary overshoot of the Japan-Sea throughflows at −5 m. These nonlinear processes are caused by the opening of the Soya Strait and thus formation of the modern EAMS-circulation structure, and a transient absence of the circulation resembling a Kuroshio Large Meander following around-island integral constraint, respectively. Conceptually, our findings introduce the around-island integral constraint on abrupt shift in the global marginal-sea circulation during the last deglaciation.

npj Climate and Atmospheric ScienceVol. 8(1)
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Qilu University of Technology (CN), University of Bremen (DE), Ministry of Natural Resources (CN), China University of Geosciences (Beijing) (CN), Institute of Oceanology (CN), Qingdao National Laboratory for Marine Science and Technology (CN), First Institute of Oceanography (CN), Shandong Academy of Sciences (CN), Laoshan Laboratory, Ocean University of China (CN)
Life below water
Openalex Percentile: Top 20%
Geophysics and Gravity Measurements
1.79
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.