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Longitudinal dependence of the H+ concentration distribution in the plasmasphere according to INTERBALL-1 satellite data
Authors:D.?V.?Chugunin  author-information"  >  author-information__contact u-icon-before"  >  mailto:dimokch@iki.rssi.ru"   title="  dimokch@iki.rssi.ru"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author,G.?A.?Kotova,M.?V.?Klimenko,V.?V.?Klimenko
Affiliation:1.Space Research Institute,Russian Academy of Sciences,Moscow,Russia;2.Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, West Department,Russian Academy of Sciences,Kaliningrad,Russia;3.Immanuel Kant Baltic Federal University,Kaliningrad,Russia
Abstract:The paper has presented a study of the dependence of the H+ ions concentration in the plasmasphere on geographic longitude. A vast database of measurements of the cold plasma density by the Alpha-3 instrument on board the INTERBALL-1 satellite has been used for the study. Based on these measurements, a dependence of the H+ ions concentration in the filled magnetic flux tube in the plasmasphere in the equatorial plane under quiet geomagnetic conditions has been obtained as a function of geographic longitude. Studies have been performed for two seasons, summer and winter. It has been shown that, during the summer in the near-midnight sector, the minimum in the H+ concentration falls within geographic longitudes of 270°–315°. The ratio of the concentration of H+ ions at various longitudes could reach a factor of three. During the winter, in the near-noon sector, the maximum of the H+ ions concentration falls within longitudes of 180°–225°, whereas the concentration ratio could reach a factor of 2.2.
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