temperature perturbations
Feb 14, 2023

Thermospheric and Ionospheric Effects by Gravity Waves from the Lower Atmosphere

Zonal wind averages from Smax simultations
Feb 14, 2023

Climate responses under an extreme quiet sun scenario

neutral density perturbation observed by CHAMP and GRACE
Dec 16, 2022

Thermospheric Density Perturbations Produced by Traveling Atmospheric Disturbances during August 2005 Storm

Lyman-alpha emission
Nov 9, 2022

Synthetic Lyman-α Emissions for the coronagraph aboard the ASO-S mission I: an Eruptive Prominence-cavity System

Latitude-longitude distribution and NmF2 simulation
Oct 18, 2022

Investigation of the Post-Sunset Extra Electron Density Peak Poleward of the Equatorial Ionization Anomaly Southern Crest

Comparisons of local time structure of molecular oxygen at 21°N, 170 km altitude
Jul 11, 2022

The Molecular Oxygen Density Structure of the Lower Thermosphere as Seen by GOLD and Models

Local-time and seasonal variations of day-to-day variability of vertical E×B drift
Nov 18, 2021

Quiet-time Day-to-day Variability of Equatorial Vertical E×B Drift from Atmosphere Perturbations at Dawn

Monthly EPB occurrence rate, obtained from daily EPB occurrence rate, which is in turn deduced from the maximum PRE using an empirical relation
Nov 18, 2021

Day-to-day variability of pre-reversal enhancement in the vertical ion drift in response to large-scale forcing from the lower atmosphere

Comparison of 135.6 nm emissions from the SAMI3/WACCM-X simulation for the March case (left and middle panels) and GOLD emission data (right panel) observed from geosynchronous orbit [Eastes et al., 2019]
Nov 17, 2021

Global Modeling of Equatorial Spread F with SAMI3/WACCM-X

Daily values of migrating diurnal tidal amplitudes (left panel) and phases (right panel) at 1E-2 hPa (80 km) from the novel multiple satellite analysis method described in this paper (upper panel), NOGAPS-ALPHA (middle panel), and WACCM-X (lower panel)
Nov 16, 2021

Day-to-Day Variability of Diurnal Tide in the Mesosphere and Lower Thermosphere Driven From Below

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