日本地球惑星科学連合2024年大会

講演情報

[E] 口頭発表

セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

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

2024年5月31日(金) 09:00 〜 10:15 展示場特設会場 (2) (幕張メッセ国際展示場 6ホール)

コンビーナ:細川 敬祐(電気通信大学大学院情報理工学研究科)、Liu Huixin(九州大学理学研究院地球惑星科学専攻 九州大学宙空環境研究センター)、大塚 雄一(名古屋大学宇宙地球環境研究所)、Chang Loren(Institute of Space Science, National Central University)、Chairperson:Jaroslav Chum(Institute of Atmospheric Physics of the Czech Academy of Sciences)、齊藤 昭則(京都大学大学院理学研究科地球物理学教室)

10:00 〜 10:15

[PEM12-25] The effects of lower atmospheric forcing and geomagnetic activity on the day-to-day variability
of the F2 region ionosphere electron densities

★Invited Papers

*Wenbin Wang1、Dong Lin1、Haonan Wu1、Jia Yue2、Jack Wang2、Xuguang Cai3 (1.National Center for Atmospheric Research、2.NASA GSFC、3.CU Boulder)

キーワード:Ionosphere, Waves, lower atmosphere-ionosphere couling, Modeling

The Earth’s F2-region ionosphere is greatly influenced by transport processes, including those by
neutral winds and electric fields. In this study, we employ the Thermosphere Ionosphere
Electrodynamics General Circulation Model (TIEGCM) to investigate the separate and combined
effects of lower atmospheric wave forcing and geomagnetic activity on F2-region ionospheric
plasma transport and electron density variability. The lower boundary of the TIEGCM is nudged
with the outputs from the Special Dynamics-Whole Atmosphere Community Climate Model
with thermosphere and ionosphere extension (SD-WACCM-X). SD-WACCM-X provides a more
realistic specification of lower atmospheric tides and planetary wavs that affect thermospheric
winds and dynamo and thereby ionospheric electron densities. We compare TIEGCM
simulations with and without SD-WACCM-X nudging and observations to assess upward
propagating lower atmospheric waves effects and the pathways by which these effects occur.
High latitude forcing is also turned on and off in these simulations for geomagnetically quiet,
moderate and storm conditions to evaluate how the lower atmospheric waves precondition and
interaction with high latitude forcing effects, and their relative roles in ionospheric day-to-day
variability.