The 18 May 2024 superbolide over the Iberian Peninsula: USG space sensors and ground-based independent observations

Abstract

On 18 May 2024, a superbolide traversed the western part of the Iberian Peninsula, culminating its flight over the Atlantic Ocean and generating significant media attention. This event was caused by a weak carbonaceous meteoroid of 93.0$\pm$0.8 cm, with a density of 1613$\pm$12 kg\,m$^{-3}$, entering the atmosphere at 40.1$\pm$0.4 km\,s$^{-1}$ with an angle of 10.93$\pm$0.02$^\circ$. The luminous phase started at 137.88$\pm$0.05 km and ended at an altitude of 53.78$\pm$0.07 km. The meteoroid's heliocentric orbit was characterized by an inclination of 14.42$\pm$0.23$^\circ$, a high eccentricity of 0.950$\pm$0.004, a semi-major axis of 2.31$\pm$0.13 au, and a notably short perihelion distance of 0.116$\pm$0.003 au. The superbolide was recorded by multiple ground-based stations of the Spanish Meteor Network (SPMN), the European Space Agency (ESA), and the U.S. Government (USG) space sensors. Our analysis shows a good agreement with the radiant and velocity data reported by the Center for Near-Earth Object Studies (CNEOS), with a deviation of 1.6$^\circ$ and -0.4 km\,s$^{-1}$, respectively. Due to the absence of observable deceleration, we successfully reconciled satellite radiometric data with a purely dynamic atmospheric flight model, constraining the meteoroid's mass and coherently fitting its velocity profile.