Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23

When the Wind spacecraft started its only journey to Lagrange point L2 in 2003 October, it entered an isotropic turbulent environment with radially mean magnetic field ( B _m ) and slow solar wind speed ( V _SW ). On October 26, it detected a particle intensity dropout interval following a gradual s...

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Main Author: Lun C. Tan
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:The Astrophysical Journal
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Online Access:https://doi.org/10.3847/1538-4357/adba50
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author Lun C. Tan
author_facet Lun C. Tan
author_sort Lun C. Tan
collection DOAJ
description When the Wind spacecraft started its only journey to Lagrange point L2 in 2003 October, it entered an isotropic turbulent environment with radially mean magnetic field ( B _m ) and slow solar wind speed ( V _SW ). On October 26, it detected a particle intensity dropout interval following a gradual solar energetic particle event. In addition, it recorded three magnetic field rotations corresponding to one-sided increases in V _SW , indicating the occurrence of magnetic switchback in the Alfvénic solar wind. Since the last switchback interval is just before the dropout interval, we studied the difference of the pitch angle distribution (PAD) of protons between them. In the switchback interval ( B _m perpendicular to V _sw ), the PAD maximum is located at μ ∼ +1, where μ is the pitch angle cosine, while, in the dropout interval ( B _m antiparallel to V _sw ), the maximum is at μ ∼ 0. The difference indicates that protons with greater gyroradii cannot be confined in the curved magnetic field lines and can be injected into the dropout region with μ ∼ 0. Therefore, the analysis of proton pitch angle scattering in the dropout interval can be greatly simplified due to the short duration of the interval and the sharp initial conditions. Compared with the analytical solution of the Fokker–Planck equation, we deduce that the parallel mean free path of 2.1 MeV protons is 3.7 ± 0.5 au, which means that the dropout of proton intensity in the isotropic turbulent regime is also caused by insufficient spatial diffusion of protons.
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spelling doaj-art-0f96149dec5d44f59362c64e407b89b42025-08-20T01:50:31ZengIOP PublishingThe Astrophysical Journal1538-43572025-01-019831410.3847/1538-4357/adba50Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23Lun C. Tan0https://orcid.org/0000-0002-7296-9174Department of Astronomy, University of Maryland , College Park, MD 20742, USA ; ltan@umd.edu; Partnership for Heliophysics and Space Environment Research (PHaSER) , USAWhen the Wind spacecraft started its only journey to Lagrange point L2 in 2003 October, it entered an isotropic turbulent environment with radially mean magnetic field ( B _m ) and slow solar wind speed ( V _SW ). On October 26, it detected a particle intensity dropout interval following a gradual solar energetic particle event. In addition, it recorded three magnetic field rotations corresponding to one-sided increases in V _SW , indicating the occurrence of magnetic switchback in the Alfvénic solar wind. Since the last switchback interval is just before the dropout interval, we studied the difference of the pitch angle distribution (PAD) of protons between them. In the switchback interval ( B _m perpendicular to V _sw ), the PAD maximum is located at μ ∼ +1, where μ is the pitch angle cosine, while, in the dropout interval ( B _m antiparallel to V _sw ), the maximum is at μ ∼ 0. The difference indicates that protons with greater gyroradii cannot be confined in the curved magnetic field lines and can be injected into the dropout region with μ ∼ 0. Therefore, the analysis of proton pitch angle scattering in the dropout interval can be greatly simplified due to the short duration of the interval and the sharp initial conditions. Compared with the analytical solution of the Fokker–Planck equation, we deduce that the parallel mean free path of 2.1 MeV protons is 3.7 ± 0.5 au, which means that the dropout of proton intensity in the isotropic turbulent regime is also caused by insufficient spatial diffusion of protons.https://doi.org/10.3847/1538-4357/adba50Interplanetary turbulenceSolar energetic particlesSolar magnetic fieldsSolar particle emissionSolar wind
spellingShingle Lun C. Tan
Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
The Astrophysical Journal
Interplanetary turbulence
Solar energetic particles
Solar magnetic fields
Solar particle emission
Solar wind
title Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
title_full Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
title_fullStr Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
title_full_unstemmed Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
title_short Proton Intensity Dropout in Isotropic Turbulence Regime during Gradual Solar Energetic Particle Events in Solar Cycle 23
title_sort proton intensity dropout in isotropic turbulence regime during gradual solar energetic particle events in solar cycle 23
topic Interplanetary turbulence
Solar energetic particles
Solar magnetic fields
Solar particle emission
Solar wind
url https://doi.org/10.3847/1538-4357/adba50
work_keys_str_mv AT lunctan protonintensitydropoutinisotropicturbulenceregimeduringgradualsolarenergeticparticleeventsinsolarcycle23