Storm-Driven Suppression and Post-Storm Enhancement of Photographic Plate Transient Detections at Geosynchronous Altitude: Empirical Evidence and a Candidate Dusty Plasma Mechanism
This paper presents empirical evidence that VASCO-project-identified sub-second optical transients at geosynchronous altitude are suppressed during geomagnetic storms and significantly enhanced in the weeks following, proposing a candidate mechanism involving storm-trapped, aggregated icy dust that reflects sunlight to explain these pre-satellite era observations.