特邀奥地利科学技术研究所Jiawei Bao博士作学术报告——大气•风云讲坛(2026年第09期)

发布单位:气候系统预测与变化应对全国重点实验室办公室、气象与环境联合研究中心、院士工作办公室 编辑:何琼发布时间:2026-04-03浏览量:

地点 气象楼423会议室 报告人 Jiawei Bao 博士
报告时间 2026-04-09 14:30:00 主持人 孙巧红 教授

报告时间:2026年4月9日(周四)14:30

报告地点:气象楼423会议室

主 持 人:孙巧红 教授

报告题目:Tropics-wide intraseasonal oscillation

报告专家:Jiawei Bao 博士

专家简介:

Jiawei Bao is Marie Curie Postdoctoral Fellow at the Institute of Science and Technology Austria (ISTA). His research focuses broadly on tropical convection and atmospheric dynamics. Dr. Bao use a combination of theory, numerical modeling, and observational data to investigate convection and its interactions with the large-scale circulation. Prior to joining ISTA, he was a postdoctoral researcher at the Max Planck Institute for Meteorology. He completed my Ph.D. in Climate Science at the University of New South Wales in Sydney, Australia. He obtained undergraduate degree from Nanjing University of Information Science and Technology and master’s degree from Beijing Normal University.。


报告摘要:

The tropical climate variability is characterized by various oscillations across a range of timescales. Oscillations that imprint the tropical mean state are generally attributed to slow processes, such as the seasonal cycle or interannual variability. Here, we identify a pronounced tropics-wide intraseasonal oscillation (TWISO) in satellite observations and reanalyses. This oscillation, with a period of 30 to 60 days, is evident across multiple variables and involves interactions between convection, radiation, surface fluxes, and large-scale circulation. It is primarily manifested as convective perturbations in the tropical Indo-Pacific warm pool accompanied by oscillations in the large-scale tropical overturning circulation. Here, we examine the relationship between TWISO, the Madden-Julian Oscillation (MJO), and the instability of radiative-convective equilibrium. Certain phases of TWISO coincide with specific phases of the MJO, suggesting a potential connection between the two. However, although the MJO can amplify the oscillation amplitude of TWISO, it is not essential for TWISO to occur. Finally, due to its broad manifestation across the tropics, TWISO potentially exerts widespread influence on tropical weather and climate at regional scales.

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