TY - JOUR
T1 - Impact of Increasing Greenhouse Gases on the Ionosphere and Thermosphere Response to a May 2024-Like Geomagnetic Superstorm
AU - Pedatella, Nicholas M.
AU - Liu, Huixin
AU - Liu, Han Li
AU - Herrington, Adam
AU - McInerney, Joseph
N1 - Publisher Copyright:
© 2025 The Author(s).
PY - 2025/6/28
Y1 - 2025/6/28
N2 - The Community Earth System Model (CESM) Whole Atmosphere Community Climate Model with thermosphere-ionosphere eXtension (WACCM-X) is used to investigate how the ionosphere-thermosphere response to a May 2024-like geomagnetic storm changes with increasing greenhouse gases. Coupled CESM(WACCM-X) simulations are first performed following the Coupled Model Intercomparison Project Phase 6 Shared Socioeconomic Pathway 5–8.5 from 2000 to 2090. The May 2024 geomagnetic superstorm is then simulated in 2016, 2040, 2061, and 2084, corresponding to surface (Formula presented.) levels of 403, 500, 652, and 918 ppmv, respectively. The CESM(WACCM-X) simulations indicate that increasing levels of (Formula presented.) weakens the absolute neutral density response at 350 km. However, the relative response is increased with increasing levels of (Formula presented.), which is partly due to the decrease in the background neutral density. Due to a weaker response in thermosphere composition and meridional neutral winds, the ionospheric response in absolute terms also weakens with increasing levels of (Formula presented.).
AB - The Community Earth System Model (CESM) Whole Atmosphere Community Climate Model with thermosphere-ionosphere eXtension (WACCM-X) is used to investigate how the ionosphere-thermosphere response to a May 2024-like geomagnetic storm changes with increasing greenhouse gases. Coupled CESM(WACCM-X) simulations are first performed following the Coupled Model Intercomparison Project Phase 6 Shared Socioeconomic Pathway 5–8.5 from 2000 to 2090. The May 2024 geomagnetic superstorm is then simulated in 2016, 2040, 2061, and 2084, corresponding to surface (Formula presented.) levels of 403, 500, 652, and 918 ppmv, respectively. The CESM(WACCM-X) simulations indicate that increasing levels of (Formula presented.) weakens the absolute neutral density response at 350 km. However, the relative response is increased with increasing levels of (Formula presented.), which is partly due to the decrease in the background neutral density. Due to a weaker response in thermosphere composition and meridional neutral winds, the ionospheric response in absolute terms also weakens with increasing levels of (Formula presented.).
KW - geomagnetic storm
KW - ionosphere
KW - thermosphere
UR - https://www.scopus.com/pages/publications/105008204891
U2 - 10.1029/2025GL116445
DO - 10.1029/2025GL116445
M3 - Article
AN - SCOPUS:105008204891
SN - 0094-8276
VL - 52
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 12
M1 - e2025GL116445
ER -