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Aaron Ridley
University of Michigan Ann ArborMeeting roles in:
Why NASA’s GDC Mission Matters: Lessons from the15 May 2005 Geomagnetic Storm
Quantifying the temporal and spatial scales in the thermosphere and ionosphere for multi-satellite mission designs
Using GOLD Data to Improve the GITM Upper Atmosphere Simulation
Assessing Modeled High‑Latitude Ionospheric Electrodynamics Using DMSP Observations
Correcting Empirical Model Densities During Geomagnetic Storms Using Commonly Available Two-Line Element Orbital Data
Advancements in Modeling the Ionosphere-Thermosphere System’s Response to Extreme Geomagnetic Storms
GITM simulation of I-T response to reversed two-cell convection during large-scale auroral precipitation in the polar cap
Development of Swirls in the Thermosphere and Ionosphere during May 2024 Storm: GITM Simulation
One Step Closer with GITM: How Lower Atmospheric Tides Control the Ionosphere-Thermosphere
Dynamic responses of ionosphere and plasmasphere during 2024 October super storm by GITM-SAMI3
Probing the Cosmic Shoreline -- Modeling the Impact of Enhanced Solar EUV and Stellar EUV spectra on Earth-like Ionospheres
Investigating the Relative Contribution of Ion Drag to Thermospheric Wind Dynamics in High-Latitude Regions During a Geomagnetic Storm: A Case Study
Assessing High-latitude Electrodynamics: Validation and Characterization of Perturbations in the Coupled Ionosphere-Thermosphere System
Exploring Cross Polar Cap Potential in Global Simulation of the Gannon Storm
Simulating the Impact of Viscosity on Thermospheric Winds and Temperature Structure During Geomagnetic Storms
Unraveling Super Equatorial Plasma Bubbles (EPBs) Development During the April 23, 2023 Storm: Multi-instrument Observations and GITM-SAMI3 Simulation
A Deep Learning-Based Model for High-Latitude Electrodynamics
Auroral Boundary Identification from IMAGE FUV Imagery: A Comparison of FTA and Global UV Imaging Methods
Wave forcing from above and below: detecting traveling atmospheric disturbances and defining gravity waves under differing geomagnetic and terrestrial forcing conditions
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