author_facet Zhou, X.‐Z.
Pu, Z. Y.
Zong, Q.‐G.
Xie, L.
Zhou, X.‐Z.
Pu, Z. Y.
Zong, Q.‐G.
Xie, L.
author Zhou, X.‐Z.
Pu, Z. Y.
Zong, Q.‐G.
Xie, L.
spellingShingle Zhou, X.‐Z.
Pu, Z. Y.
Zong, Q.‐G.
Xie, L.
Journal of Geophysical Research: Space Physics
Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
author_sort zhou, x.‐z.
spelling Zhou, X.‐Z. Pu, Z. Y. Zong, Q.‐G. Xie, L. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2006ja012180 <jats:p>Several mechanisms have been used to explain solar wind plasma entry into the plasma sheet in the magnetotail. In this paper, we focus on the gradient drift entry (GDE) process in the equatorial flanks of the magnetosphere, based on the magnetopause picture of a tangential discontinuity with a small tangential electric field as was suggested by Alfvén (1968). We discuss the GDE efficiency in different conditions using the adiabatic theory. It can be clearly shown that the GDE efficiency is much lower during southward interplanetary magnetic field (IMF), with a strong energy filter effect for incoming solar wind particles. Given a typical condition, a critical energy for particle entry is calculated to be several kiloelectron volts. Only those particles with higher energy can penetrate the magnetopause, a condition which can be also proved by test particle simulations. The lower efficiency than that during northward IMF during periods of southward IMF is in agreement with the different properties of the plasma sheet observed, i.e., hot and tenuous when the IMF is southward, cold and dense for northward IMF.</jats:p> Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field Journal of Geophysical Research: Space Physics
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Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
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Geologie und Paläontologie
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series Journal of Geophysical Research: Space Physics
source_id 49
title Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_unstemmed Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_full Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_fullStr Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_full_unstemmed Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_short Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_sort energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
topic Paleontology
Space and Planetary Science
Earth and Planetary Sciences (miscellaneous)
Atmospheric Science
Earth-Surface Processes
Geochemistry and Petrology
Soil Science
Water Science and Technology
Ecology
Aquatic Science
Forestry
Oceanography
Geophysics
url http://dx.doi.org/10.1029/2006ja012180
publishDate 2007
physical
description <jats:p>Several mechanisms have been used to explain solar wind plasma entry into the plasma sheet in the magnetotail. In this paper, we focus on the gradient drift entry (GDE) process in the equatorial flanks of the magnetosphere, based on the magnetopause picture of a tangential discontinuity with a small tangential electric field as was suggested by Alfvén (1968). We discuss the GDE efficiency in different conditions using the adiabatic theory. It can be clearly shown that the GDE efficiency is much lower during southward interplanetary magnetic field (IMF), with a strong energy filter effect for incoming solar wind particles. Given a typical condition, a critical energy for particle entry is calculated to be several kiloelectron volts. Only those particles with higher energy can penetrate the magnetopause, a condition which can be also proved by test particle simulations. The lower efficiency than that during northward IMF during periods of southward IMF is in agreement with the different properties of the plasma sheet observed, i.e., hot and tenuous when the IMF is southward, cold and dense for northward IMF.</jats:p>
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author Zhou, X.‐Z., Pu, Z. Y., Zong, Q.‐G., Xie, L.
author_facet Zhou, X.‐Z., Pu, Z. Y., Zong, Q.‐G., Xie, L., Zhou, X.‐Z., Pu, Z. Y., Zong, Q.‐G., Xie, L.
author_sort zhou, x.‐z.
container_issue A6
container_start_page 0
container_title Journal of Geophysical Research: Space Physics
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description <jats:p>Several mechanisms have been used to explain solar wind plasma entry into the plasma sheet in the magnetotail. In this paper, we focus on the gradient drift entry (GDE) process in the equatorial flanks of the magnetosphere, based on the magnetopause picture of a tangential discontinuity with a small tangential electric field as was suggested by Alfvén (1968). We discuss the GDE efficiency in different conditions using the adiabatic theory. It can be clearly shown that the GDE efficiency is much lower during southward interplanetary magnetic field (IMF), with a strong energy filter effect for incoming solar wind particles. Given a typical condition, a critical energy for particle entry is calculated to be several kiloelectron volts. Only those particles with higher energy can penetrate the magnetopause, a condition which can be also proved by test particle simulations. The lower efficiency than that during northward IMF during periods of southward IMF is in agreement with the different properties of the plasma sheet observed, i.e., hot and tenuous when the IMF is southward, cold and dense for northward IMF.</jats:p>
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imprint American Geophysical Union (AGU), 2007
imprint_str_mv American Geophysical Union (AGU), 2007
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publishDate 2007
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spelling Zhou, X.‐Z. Pu, Z. Y. Zong, Q.‐G. Xie, L. 0148-0227 American Geophysical Union (AGU) Paleontology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Atmospheric Science Earth-Surface Processes Geochemistry and Petrology Soil Science Water Science and Technology Ecology Aquatic Science Forestry Oceanography Geophysics http://dx.doi.org/10.1029/2006ja012180 <jats:p>Several mechanisms have been used to explain solar wind plasma entry into the plasma sheet in the magnetotail. In this paper, we focus on the gradient drift entry (GDE) process in the equatorial flanks of the magnetosphere, based on the magnetopause picture of a tangential discontinuity with a small tangential electric field as was suggested by Alfvén (1968). We discuss the GDE efficiency in different conditions using the adiabatic theory. It can be clearly shown that the GDE efficiency is much lower during southward interplanetary magnetic field (IMF), with a strong energy filter effect for incoming solar wind particles. Given a typical condition, a critical energy for particle entry is calculated to be several kiloelectron volts. Only those particles with higher energy can penetrate the magnetopause, a condition which can be also proved by test particle simulations. The lower efficiency than that during northward IMF during periods of southward IMF is in agreement with the different properties of the plasma sheet observed, i.e., hot and tenuous when the IMF is southward, cold and dense for northward IMF.</jats:p> Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field Journal of Geophysical Research: Space Physics
spellingShingle Zhou, X.‐Z., Pu, Z. Y., Zong, Q.‐G., Xie, L., Journal of Geophysical Research: Space Physics, Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field, Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
title Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_full Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_fullStr Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_full_unstemmed Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_short Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_sort energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
title_unstemmed Energy filter effect for solar wind particle entry to the plasma sheet via flank regions during southward interplanetary magnetic field
topic Paleontology, Space and Planetary Science, Earth and Planetary Sciences (miscellaneous), Atmospheric Science, Earth-Surface Processes, Geochemistry and Petrology, Soil Science, Water Science and Technology, Ecology, Aquatic Science, Forestry, Oceanography, Geophysics
url http://dx.doi.org/10.1029/2006ja012180