*Li Lo1,2、Simon T. Belt3、Julie Lattaud4、Axel Timmermann5,6、Christian Zeeden7、Stefan Schouten4,8、Lukas Smik3、Tobias Friedrich6、Patricia Cabedo-Sanz3、Jyh-Jaan Huang9、Liping Zhou10、Tsong-Hua Ou11、Yuan-Ping Chang12、Liang-Chi Wang13、Yu-Min Chou9、Chuan-Chou Shen9、Min-Te Chen14、Kuo-Yen Wei9、Sheng-Rong Song9、Tien-Hsi Fang14、Sergey A. Gorbarenko15、Wei-Lung Wang16、Teh-Quei Lee17、Henry Elderfield1、David A. Hodell1 (1.Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge、2.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochecmistry, Chinese Academy of Sciences、3.Biogeochemical Research Centre, School of Geography, Earth and Environmental Sciences, Plymouth University、4.NIOZ, Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, and Utrecht University、5.nstitute of Basic Science, Center for Climate Physics, Pusan National University、6.International Pacific Research Center, School of Ocean and Earth Science and Technology, University of Hawaii、7.Lehrstuhl für Physische Geographie und Geoökologie, RWTH Aachen University、8.Faculty of Geosciences, Department of Earth Sciences, Utrecht University、9.Department of Geosciences, National Taiwan University、10.College of Urban and Environmental Sciences, Peking University、11.Institute of Applied Mechanics, National Taiwan University、12.Department of Oceanography, National Sun Yat-sen University、13.Collection Management Department, National Taiwan Museum、14.Institute of Applied Geosciences, National Taiwan Ocean University、15.V.I. II'ichev Pacific Oceanological Institute, Far East Branch Russian Academy of Science、16.Department of Biology, National Changhua University of Education、17.Institute of Earth Sciences, Academia Sinica)
セッション情報
[EE]Evening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] [EE] アジア・モンスーンの進化と変動、新生代寒冷化との関係
2017年5月23日(火) 17:15 〜 18:30 ポスター会場 (国際展示場 7ホール)
Although Asian Monsoon (AM) is a regional phenomenon, it exerts a significant impact on the global climate. Since uplift of Himalaya and Tibetan Plateau (HTP) has been considered to have played a significant role on the establishment and intensification of AM, numerous attempts have been made to prove the linkage between the HTP uplift and AM evolution, but the linkage is largely unproved till now. On the other hand, comparison of global climatic changes, pCO2 reconstructions, and AM evolution process during Cenozoic suggests that AM evolution is significantly affected by global climate changes most likely through pCO2. Thus, importance of the HTP uplift on AM evolution is questioned. However, it should be noted that the effects of the HTP uplift and AM precipitation on chemical weathering, erosion, and CO2 uptake could be acting as feedback loops on AM-HTP uplift linkage.
From July 2013 to November 2016, IODP conducted a series of expeditions such as 346 (Asian Monsoon), 353 (Indian Monsoon Rainfall), 354 (Bengal Fan), 355 (Arabian Monsoon), 356 (Indian through-flow), and 359 (Maldives Monsoon) that are related to AM evolution and its interaction with global climate system in NW Pacific and Indian Ocean regions, and exciting results are gradually coming out. We believe it is timely to start gathering and synthesizing the results of these cruises and update and exchange information and ideas to promote our understanding of AM evolution, variability, their controlling factors, and their interaction with global climate system during the Cenozoic.
*Xingyan Shen1,2、Shiming Wan1 (1.Institute of Oceanology, Chinese Academy of Sciences、2.University of Chinese Academy of Sciences)
*臼井 洋一1、Taylor Samuel2 (1.海洋研究開発機構、2.Institut de Physique du Globe de Paris)