Artificial plasma cloud evolution in the low latitude ionosphere

Details Artificial plasma cloud evolution in the low latitude ionosphere Artificial plasma cloud evolution in the low latitude ionosphere

Feb 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993jatp...55..193k&link_type=abstract

Journal of Atmospheric and Terrestrial Physics (ISSN 0021-9169), vol. 55, no. 2, p. 193-195.

Physics

2

Barium Ion Clouds, Earth Ionosphere, Equatorial Atmosphere, Plasma Drift, Earth Magnetosphere, Rocket-Borne Instruments, Solar Radiation

Scientific paper

Artificial plasma cloud evolution in the low-latitude ionosphere was studied in the Contrast-3 active rocket experiment carried out on August 21, 1991 at 18 deg N, 53.2 deg W. The ionized barium cloud was observed at dawn the next day, more than 10 h after the barium injection. The barium cloud traveled northeastward. When moving, the cloud significantly varied its visible structure. The observed cloud deformation is argued to be caused by variations in the observational angle as well as by different travel speeds of its separate structures.

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