*Steven C Clemens1, Masanobu Yamamoto2, Sarah McGrath1, Kaustubh Thirumalai3, Yongsong Huang1, Kerr Katrina 4, Richey Julie 5, Rosenthal Yair6 (1.Brown University, 2.Hokkaido University, 3.University of Arizona, 4.Open University, 5.USGS, 6.Rutgers University)
Session information
[E] Oral
M (Multidisciplinary and Interdisciplinary) » M-IS Intersection
[M-IS05] Cenozoic Evolution of the Asian Monsoon and the Indo-Pacific Paleoclimates
convener:Masanobu Yamamoto(Faculty of Environmental Earth Science, Hokkaido University), Steven C Clemens(Brown University), Hongbo Zheng(Research Center for Earth System Science, Yunnan University), Ryuji Tada(Department of Earth and Planetary Science, Graduate School of Science, The Univeristy of Tokyo)
The Asian monsoon (AM) and the El Nino-Southern Oscillation (ENSO) are dominant atmospheric-ocean phenomena on the Earth and affect the climates of Asia, Oceania and circum-Pacific regions. During the Cenozoic, the climate of these areas changed drastically, but the behaviors of the Asian monsoon and the tropical ocean-atmosphere interactions like the ENSO were not fully understood. From July 2013 to December 2016, IODP conducted a series of expeditions such as 346 (Asian Monsoon), 353 (Indian Monsoon Rainfall), 354 (Bengal Fan), 355 (Arabian Sea Monsoon), 356 (Indonesian Throughflow), 359 (Maldives Monsoon and Sea Level), 361 (Southern African Climate), and 363 (Western Pacific Warm Pool) that are related to the AM and tropical Pacific climate evolution and its interaction with global climate system in NW and tropical Pacific and Indian Ocean regions, and exciting results are coming out. We believe it is timely to start synthesizing the results of these cruises and update and exchange information and ideas to promote our understanding of the AM and tropical Pacific evolution, variability, their controlling factors, and their interaction with global climate system during the Cenozoic. On orbital and millennial timescales, studies on the response of the AM and the ENSO to climate forcing are intensively studied using various archives such as sediments, speleothems, corals, etc., during the last decade. Presentations and discussions on the above topics from various backgrounds (proxy and modeling studies) are highly welcome.
*Tomohisa Irino1, Masanobu Yamamoto1, Liviu Giosan2, Steven Clemens3 (1.Faculty of Environmental Earth Science, Hokkaido University, 2.Woods Hole Institution of Oceanography, 3.Brown University)
*Mui Fa Alison Lee1, Tomohisa Irino1 (1.Faculty of Environmental Earth Science, Hokkaido University)
*Ran Zhang1 (1.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China )
*Hongbo Zheng1, Qing Yang1, Shuo Cao3, Peter Dominic Clift4, Mengying He2, Akihiro Kano5, Ryuji Tada5, Fred Jourdan6 (1.Research Center for Earth System Science, Yunnan University, 2.School of Geography Science, Nanjing Normal University, 3.School of Earth Sciences, China University of Geosciences, 4.Department of Geology and Geophysics, Louisiana State University, 5.Department of Earth and Planetary Science, University of Tokyo, 6.Western Australian Argon Isotope Facility, Department of Applied Geology and JdL Centre, Curtin University)