Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG38] Multi-scale ocean-atmosphere interaction in the tropical Indo-Pacific region

Tue. May 28, 2019 9:00 AM - 10:30 AM 104 (1F)

convener:Ayako Seiki(Japan Agency for Marine-Earth Science and Technology), Tomoki Tozuka(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Motoki Nagura(Japan Agency for Marine-Earth Science and Technology), Youichi Kamae(Faculty of Life and Environmental Sciences, University of Tsukuba), Chairperson:Ayako Seiki(Japan Agency for Marine-Earth Science and Technology), Motoki Nagura(Japan Agency for Marine-Earth Science and Technology)

10:00 AM - 10:15 AM

[ACG38-05] Impact of atmospheric variability on Indian Ocean Dipole mode

*Yuya Baba1 (1.JAMSTEC Japan Agency for Marine-Earth Science and Technology)

Keywords:Indian Ocean Dipole mode, atmospheric internal variability

Some preceding studies investigated tropical atmospheric internal variability such as Madden-Julian oscillation on the formation of Indian Ocean Dipole mode (IOD), but still number of the studies remains few, and their relationship remains unknown. In this study, we focused on the impact of atmospheric variability especially intraseasonal variability. To reveal the impact, we conducted sensitivity experiments for the IOD during 1980-2009, using an ocean general circulation model and difference atmospheric forcing data, such as (1) climatological forcing, (2) same as (1) but with yearly anomalies, (3) same as (1) but with seasonal anomalies, (4) same as (1) but with monthly anomalies, (5) 90-day low-pass filtered forcing. The simulated Dipole mode index (DMI) indicates that the sensitivity case of (1) could not reproduced realistic DMI at all, (2) and (3) reproduced decreased DMI amplitudes, and (4) and (5) reproduced similar DMI which was simulated with daily forcing data. In this presentation, possible mechanisms that caused different features of simulated IODs will be explained, focusing on the relationship between the variabilities of ocean and atmosphere.