[P-EM12] Coupling Processes in the Atmosphere-Ionosphere System

[PEM12-39] Intraseasonal Variability of the Equatorial Ionosphere Responses to the Madden-Julian Oscillation

*Xu Zhou¹、Guiwan Chen²、Xinan Yue¹、Ruilong Zhang¹、Akimasa Yoshikawa³ (1.Institute of Geology and Geophysics, Chinese Academy of Sciences、2.Institute of Atmospheric Physics, Chinese Academy of Sciences、3.Department of Earth and Planetary Sciences, Kyushu University)

キーワード：Equatorial Ionosphere, Plasma Drifts, Madden-Jullian Oscillation, Whole Atmosphere Simulation, Atmospheric Tides

This study investigates the response of the equatorial ionosphere to the tropospheric Madden-Jullian Oscillation (MJO) using the Whole Atmosphere Community Climate Model-eXtended (WACCM-X). The main results indicate that the intraseasonal variability of ionospheric vertical plasma drifts (V_iz) is generally strong around boreal winters and exhibits significant eastward-propagating signals. Composite analysis showed that, during the December-January-February-March (DJFM) season, V_iz was generally negative when the MJO was active over the Maritime Continent (phase 5) and positive when the MJO was active over the Indian Ocean (phase 2). The magnitude of MJO impact on V_iz achieves ~1.2 m/s, representing roughly 10% of the seasonal mean. The eastward-propagating wavenumber-4 is apparently strong during MJO phases 5 and 1–2, which is examined to be associated with non-migrating tides below. Term analysis revealed the importance of zonal winds in driving the V_iz responses. This study emphasizes the importance of tropospheric sources that affect the geospace environment.