Overview
- An NSF NCAR-led study finds that increasing carbon dioxide cools and thins the thermosphere and ionosphere, changing storm-time atmospheric responses.
- Future storms of the same intensity are projected to reach 20–50% lower peak densities yet produce nearly triple jumps relative to the pre-storm baseline.
- The altered response could intensify episodic drag on spacecraft, affecting orbits, lifetimes, and services such as GPS and communications.
- Researchers simulated the May 10–11, 2024 superstorm for 2016, 2040, 2061, and 2084 using the CESM WACCM-X model on the Derecho supercomputer.
- The work, published in Geophysical Research Letters with Kyushu University collaborators, calls for broader assessments across storm types and solar-cycle phases.