Electron radiation belt dynamics during magnetic storms and in quiet time

The paper discusses the outer electron belt dynamics, adiabatic and nonadiabatic mechanisms of increases and losses of energetic electrons. Under undisturbed conditions, the outer electron belt gradually empties: in the inner magnetosphere due to electron losses in the atmosphere and in the quasi-t...

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Main Authors: Lazutin L.L., Dmitriev A.V., Suvorova A.V.
Format: Article
Language:English
Published: INFRA-M 2018-03-01
Series:Solar-Terrestrial Physics
Subjects:
Online Access:https://naukaru.ru/ru/nauka/article/20507/view
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author Lazutin L.L.
Dmitriev A.V.
Suvorova A.V.
author_facet Lazutin L.L.
Dmitriev A.V.
Suvorova A.V.
author_sort Lazutin L.L.
collection DOAJ
description The paper discusses the outer electron belt dynamics, adiabatic and nonadiabatic mechanisms of increases and losses of energetic electrons. Under undisturbed conditions, the outer electron belt gradually empties: in the inner magnetosphere due to electron losses in the atmosphere and in the quasi-trapping region due to losses at the magnetopause because drift shells of electrons are not closed there. The latter process does not occur in normal years due to the masking replenishment by freshly accelerated particles, but in years of extremely low activity it leads to a significant decrease in the electron population of the belt. During the magnetic storm main phase, the first reason for the decrease in the electron flux intensity is the adiabatic cooling associated with conservation of adiabatic invariants and complemented by injection of electrons into the atmosphere and their losses at the magnetopause. Electron flux increases involve EB electron injection by the induction electric field of substorm activation and by the large-scale solar wind electric field, with pitch energy diffusion along with adiabatic heating in the recovery phase. The rate of electron flux recovery after a storm is determined by the ratio of nonadiabatic increases and losses; hence the electron flux represents a continuous series from low to very high values. The combination of these processes determines the individual character of radiation belt development during each magnetic storm and the behavior of the belt in the quiet time.
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spelling doaj.art-d436b4850bf44485a3f2574c062cb3302022-12-22T03:27:28ZengINFRA-MSolar-Terrestrial Physics2500-05352018-03-0141516010.12737/stp-41201805Electron radiation belt dynamics during magnetic storms and in quiet timeLazutin L.L.0Dmitriev A.V.1Suvorova A.V.2Scobeltsyn Institute of Nuclear Physics, Moscow State University Moscow, RussiaScobeltsyn Institute of Nuclear Physics, Moscow State University Moscow, RussiaScobeltsyn Institute of Nuclear Physics, Moscow State University Moscow, RussiaThe paper discusses the outer electron belt dynamics, adiabatic and nonadiabatic mechanisms of increases and losses of energetic electrons. Under undisturbed conditions, the outer electron belt gradually empties: in the inner magnetosphere due to electron losses in the atmosphere and in the quasi-trapping region due to losses at the magnetopause because drift shells of electrons are not closed there. The latter process does not occur in normal years due to the masking replenishment by freshly accelerated particles, but in years of extremely low activity it leads to a significant decrease in the electron population of the belt. During the magnetic storm main phase, the first reason for the decrease in the electron flux intensity is the adiabatic cooling associated with conservation of adiabatic invariants and complemented by injection of electrons into the atmosphere and their losses at the magnetopause. Electron flux increases involve EB electron injection by the induction electric field of substorm activation and by the large-scale solar wind electric field, with pitch energy diffusion along with adiabatic heating in the recovery phase. The rate of electron flux recovery after a storm is determined by the ratio of nonadiabatic increases and losses; hence the electron flux represents a continuous series from low to very high values. The combination of these processes determines the individual character of radiation belt development during each magnetic storm and the behavior of the belt in the quiet time.https://naukaru.ru/ru/nauka/article/20507/viewmagnetosphereelectronsradiation beltreplenishment and losses
spellingShingle Lazutin L.L.
Dmitriev A.V.
Suvorova A.V.
Electron radiation belt dynamics during magnetic storms and in quiet time
Solar-Terrestrial Physics
magnetosphere
electrons
radiation belt
replenishment and losses
title Electron radiation belt dynamics during magnetic storms and in quiet time
title_full Electron radiation belt dynamics during magnetic storms and in quiet time
title_fullStr Electron radiation belt dynamics during magnetic storms and in quiet time
title_full_unstemmed Electron radiation belt dynamics during magnetic storms and in quiet time
title_short Electron radiation belt dynamics during magnetic storms and in quiet time
title_sort electron radiation belt dynamics during magnetic storms and in quiet time
topic magnetosphere
electrons
radiation belt
replenishment and losses
url https://naukaru.ru/ru/nauka/article/20507/view
work_keys_str_mv AT lazutinll electronradiationbeltdynamicsduringmagneticstormsandinquiettime
AT dmitrievav electronradiationbeltdynamicsduringmagneticstormsandinquiettime
AT suvorovaav electronradiationbeltdynamicsduringmagneticstormsandinquiettime