日本地球惑星科学連合2025年大会

セッション情報

[E] ポスター発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS06] Evolution and variability of the Tropical Monsoon and Indo-Pacific climate during the Cenozoic Era

2025年5月29日(木) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:松崎 賢史(東京大学 大気海洋研究所)、佐川 拓也(金沢大学理工研究域)、Ho Sze Ling(Institute of Oceanography, National Taiwan University)、Gallagher Stephen J(University of Melbourne)

The tropical monsoon system spans the African, Indian, Australian, and East Asian Monsoons. Driven by ocean-land thermal contrasts, it interacts with the global climate system. On tectonic time scales, the uplift of the Himalayas and Tibetan Plateau has been considered a significant factor in the establishment and intensification of tropical monsoon, though its importance remains debated. Paleoclimate records suggest that monsoon evolution during the Cenozoic era was also substantially influenced by global climate changes related to changes in atmospheric CO2.
The Indo-Pacific oceanography also plays a crucial role in generating land-ocean thermal contrast and water vapor circulation. The region's West Pacific Warm Pool (WPWP), the largest heat reservoir in the global ocean, significantly contributes to atmospheric heat and moisture, influencing the El Nino-Southern Oscillation (ENSO) climate pattern. The constriction of the Indonesian Seaways during the Neogene has had a major impact on the formation of the WPWP and consequently affects ENSO dynamics. However, the precise timing and mechanism of this process are still under debate.
This session aims to assess the relative importance of these processes on different time scales, from millennial to tectonic. The goal is to enhance our understanding of the evolution of the tropical Monsoon, WPWP, and ENSO variability. It also seeks to explore the controlling factors and interactions with the global climate system. Presentations based on various archives such as piston cores, DSDP/ODP/IODP cores, and land sections are encouraged. These studies welcome a broad range of paleo-environmental proxies, including geochemistry, geophysics, sedimentology, and micropaleontology. Modeling studies are also welcome to complement the proxy-based research.

17:15 〜 19:15

*松崎 賢史1板木 拓也2、久保田 好美3、Kyung Eun Lee4本山 功5佐川 拓也6堀川 恵司7村山 雅史8小畑 元1 (1.東京大学 大気海洋研究所、2.産業技術総合研究所、3.国立科学博物館、4.Korea Maritime and Ocean University、5.山形大学 理学部、6.金沢大学 理工学域、7.富山大学 理学部、8.高知大学 農林海洋科学部)

17:15 〜 19:15

*高田 裕行1池原 実2、瀬戸 浩二3、朝日 博文4、Lim Hyoun Soo5、Hyun Sangmin6、Khim Boo-Keun7 (1.BK21 School of Earth and Environmental Systems, Pusan National University、2.Marine Core Research Institute, Kochi University、3.Estuary Research Center, Shimane University、4.Fukui Prefectural Satoyama-Satoumi Research Institute、5.Department of Geological Science, Pusan National University、6.Marine Environmental Research Division, Korea Institute of Ocean Science and Technology、7.Deparment of Oceanography, Pusan National University)

17:15 〜 19:15

*関 有沙1入野 智久2多田 隆治3松崎 賢史4吉岡 純平5 (1.信州大学 理学部、2.北海道大学 大学院地球環境科学研究院、3.千葉工業大学 地球学研究センター、4.東京大学 大気海洋研究所、5.産業技術総合研究所 地質情報研究部門)

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