Empirical model of the high-latitude boundary of the Earth’s outer radiation belt at altitudes of up to 1000 km

• Published in: Cosmic research 2018, Vol.56 (1), p.32-37
• Main Authors: Kalegaev, V. V., Barinova, W. O., Myagkova, I. N., Eremeev, V. E., Parunakyan, D. A., Nguyen, M. D., Barinov, O. G.
• Format: Article
• Language: English
• Subjects: Astronomy; Astrophysics and Astroparticles; Astrophysics and Cosmology; Corona; Coronas; Earth rotation; Electron density; Electron flux; Empirical models; Equator; Geomagnetic activity; Geomagnetism; Intersections; Jupiter; Latitude; Magnetic fields; Mathematical models; Numerical analysis; Outer radiation belt; Physics; Physics and Astronomy; Radiation; Satellites; Space Exploration and Astronautics; Space Sciences (including Extraterrestrial Physics; Time dependence; Trapped electrons; Universal time
• ISSN: 0010-9525; 1608-3075
• DOI: 10.1134/S0010952518010069

An empirical model of the high-latitude boundary of the outer Earth’s radiation belt (ERB) has been presented, which is based on the measurement data of electron fluxes on the polar low-orbit CORONAS-Photon, Meteor-M1 , and Meteor-M2 satellites. The boundary was determined by a sharp decrease to the background level of the flux of trapped electrons with energies of 100 or 200 keV in the polar part of the profile of the outer radiation belt. A numerical algorithm has been implemented to determine the time moment, when the fastest flux changes are recorded. The primary search was carried out, first, on 30 s averaged data, then repeated on data with a higher resolution. A functional dependence was obtained in order to approximate the obtained set of intersections of the boundary by elliptical curve. The empirical model constructed using the CORONAS-Photon measurement data in the epoch of anomalously low geomagnetic activity reflects the longitude structure of the high-latitude boundary of the outer radiation belt associated with the internal Earth’s magnetic field (MF), as well as its dependence on the universal time. Based on the data of intersections of the high-latitude boundary of the outer ERB (OERB) in the epoch of 2014–2016, the latitudinal shift of the boundary to the equator dependent on geomagnetic activity has been determined, as well as the nightside shift of the boundary due to the diurnal rotation of the Earth.