Articles | Volume 40, issue 4
Ann. Geophys., 40, 519–530, 2022
https://doi.org/10.5194/angeo-40-519-2022
Ann. Geophys., 40, 519–530, 2022
https://doi.org/10.5194/angeo-40-519-2022
Regular paper
02 Aug 2022
Regular paper | 02 Aug 2022

Arecibo measurements of D-region electron densities during sunset and sunrise: implications for atmospheric composition

Carsten Baumann et al.

Data sets

Arecibo measurements of D-region electron 330 densities during sunset and sunrise in August 2016 C. Baumann, A. Kero, S. Raizada, M. Rapp, M. P. Sulzer, P. T. Verronen, and J. Vierinen https://doi.org/10.5281/zenodo.6381903

Download
Short summary
The Arecibo radar was used to probe free electrons of the ionized atmosphere between 70 and 100 km altitude. This is also the altitude region were meteors evaporate and form secondary particulate matter, the so-called meteor smoke particles (MSPs). Free electrons attach to these MSPs when the sun is below the horizon and cause a drop in the number of free electrons, which are the subject of these measurements. We also identified a different number of free electrons during sunset and sunrise.