The Kuroshio Current Was Stronger During the Last Glacial Maximum Than the Holocene: Evidence From Zonal Subsurface Temperature Transects

Ru-Yun Tung

Presentation information

[E] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS04] Paleoclimatology and paleoceanography

Mon. May 25, 2026 10:45 AM - 12:15 PM Exhibition Hall Special Setting (5) (Exhibition Hall 7&8, Makuhari Messe)

Chairperson:Yamazaki Atsuko(Graduate School of Environmental Studies, Nagoya University), Hasegawa Hitoshi(Faculty of Science and Technology, Kochi University), Westerhold Thomas(Center for Marine Environmental Sciences of the University of Bremen, Bremen, Germany), Nana Yobo Lucien(Texas A&M University College Station), Obase Takashi(Japan Agency for Marine-Earth Science and Technology)

10:45 AM - 11:00 AM

[MIS04-07] The Kuroshio Current Was Stronger During the Last Glacial Maximum Than the Holocene: Evidence From Zonal Subsurface Temperature Transects

*Ru-Yun Tung¹, Sze Ling Ho¹, Yuan-Pin Chang², Sam Sherriff-Tadano³, Xinyu Guo⁴, Pei-Ting Lee¹, Pierrick Fenies¹, Takuya Sagawa⁵, Chuan-Chou Shen⁶, Pei-Ling Wang¹, Yurika Ujiié⁷ (1. Institute of Oceanography, National Taiwan University, Taiwan, 2. Department of Oceanography, National Sun Yat-sen University, Taiwan , 3. Department of Physics and Earth Sciences, University of the Ryukyus, Japan, 4. Center for Marine Environmental Studies, Ehime University, Japan, 5. Institute of Science and Engineering, Kanazawa University, Japan, 6. High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taiwan, 7. Marine Core Research Institute, Kochi University, Japan)

Keywords:Kuroshio Current, Mg/Ca, δ18O