author_facet Zong, Q.‐G.
Fritz, T. A.
Spence, H.
Oksavik, K.
Pu, Z.‐Y.
Korth, A.
Daly, P. W.
Zong, Q.‐G.
Fritz, T. A.
Spence, H.
Oksavik, K.
Pu, Z.‐Y.
Korth, A.
Daly, P. W.
author Zong, Q.‐G.
Fritz, T. A.
Spence, H.
Oksavik, K.
Pu, Z.‐Y.
Korth, A.
Daly, P. W.
spellingShingle Zong, Q.‐G.
Fritz, T. A.
Spence, H.
Oksavik, K.
Pu, Z.‐Y.
Korth, A.
Daly, P. W.
Journal of Geophysical Research: Space Physics
Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
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 zong, q.‐g.
spelling Zong, Q.‐G. Fritz, T. A. Spence, H. Oksavik, K. Pu, Z.‐Y. Korth, A. Daly, P. W. 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/10.1029/2003ja009929 <jats:p>In this paper we present new results using Cluster/Research with Adaptive Particle Imaging Detectors (RAPID) energetic particle observations to remotely sound the high‐latitude magnetopause in three dimensions. We demonstrate that energetic particle flux variations in the vicinity of the magnetopause (inside the magnetosphere) are mainly modulated by the absorbing magnetopause during quiet geomagnetic conditions. Less than two gyro radii from an absorbing boundary a trapped particle distribution becomes nongyrotropic, as particles start to encounter the boundary. Knowing the magnetic field and the particle mass and energy, the direction and distance to the magnetopause can be derived by examining the azimuthal distribution of locally mirroring particles. Combining observations from three nearby spacecraft gives a three‐dimensional, local picture of the magnetopause surface. We exploit anisotropic ion distributions to determine magnetopause distances, orientations, and structures in the interval from 1320 to 1420 UT on 14 January 2001 for the three Cluster spacecraft (Rumba, Samba, and Tango) located on the duskside (at ∼1700 MLT) high‐latitude region. The results clearly illustrate that the magnetopause ion sounding technique as proposed by <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0026"><jats:italic>Williams</jats:italic> [1979]</jats:ext-link>, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0006"><jats:italic>Fritz and Fahnenstiel</jats:italic> [1982]</jats:ext-link>, and <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0028"><jats:italic>Zong et al.</jats:italic> [2000]</jats:ext-link> can be used to remotely study the three‐dimensional orientation and location of the magnetopause surface and the gradient variation of the plasma parameters. Intercomparison between energetic particle sounding distance and simultaneous plasma and magnetic field measurements suggests that solar wind plasma can penetrate more than ≈1000 km deeper than the trapping boundary. The fluxes of different ion species are proportional to the distance from the magnetopause, with a correlation coefficient of 0.7 to 0.8. The energetic proton flux gradient as a function of distance from the magnetosphere is about 100 particles cm<jats:sup>−2</jats:sup> s<jats:sup>−1</jats:sup> sr<jats:sup>−1</jats:sup> per kilometer. In contrast, the solar wind plasma density is found to be inversely proportional to the distance. The solar wind plasma appears to be bounded by an exponential with an e‐folding distance of 1000 km.</jats:p> Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID Journal of Geophysical Research: Space Physics
doi_str_mv 10.1029/2003ja009929
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finc_class_facet Chemie und Pharmazie
Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
Biologie
Allgemeine Naturwissenschaft
Physik
Technik
Geologie und Paläontologie
Geographie
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recordtype ai
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series Journal of Geophysical Research: Space Physics
source_id 49
title Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_unstemmed Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_full Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_fullStr Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_full_unstemmed Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_short Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_sort energetic particle sounding of the magnetopause: a contribution by cluster/rapid
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/10.1029/2003ja009929
publishDate 2004
physical
description <jats:p>In this paper we present new results using Cluster/Research with Adaptive Particle Imaging Detectors (RAPID) energetic particle observations to remotely sound the high‐latitude magnetopause in three dimensions. We demonstrate that energetic particle flux variations in the vicinity of the magnetopause (inside the magnetosphere) are mainly modulated by the absorbing magnetopause during quiet geomagnetic conditions. Less than two gyro radii from an absorbing boundary a trapped particle distribution becomes nongyrotropic, as particles start to encounter the boundary. Knowing the magnetic field and the particle mass and energy, the direction and distance to the magnetopause can be derived by examining the azimuthal distribution of locally mirroring particles. Combining observations from three nearby spacecraft gives a three‐dimensional, local picture of the magnetopause surface. We exploit anisotropic ion distributions to determine magnetopause distances, orientations, and structures in the interval from 1320 to 1420 UT on 14 January 2001 for the three Cluster spacecraft (Rumba, Samba, and Tango) located on the duskside (at ∼1700 MLT) high‐latitude region. The results clearly illustrate that the magnetopause ion sounding technique as proposed by <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0026"><jats:italic>Williams</jats:italic> [1979]</jats:ext-link>, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0006"><jats:italic>Fritz and Fahnenstiel</jats:italic> [1982]</jats:ext-link>, and <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0028"><jats:italic>Zong et al.</jats:italic> [2000]</jats:ext-link> can be used to remotely study the three‐dimensional orientation and location of the magnetopause surface and the gradient variation of the plasma parameters. Intercomparison between energetic particle sounding distance and simultaneous plasma and magnetic field measurements suggests that solar wind plasma can penetrate more than ≈1000 km deeper than the trapping boundary. The fluxes of different ion species are proportional to the distance from the magnetopause, with a correlation coefficient of 0.7 to 0.8. The energetic proton flux gradient as a function of distance from the magnetosphere is about 100 particles cm<jats:sup>−2</jats:sup> s<jats:sup>−1</jats:sup> sr<jats:sup>−1</jats:sup> per kilometer. In contrast, the solar wind plasma density is found to be inversely proportional to the distance. The solar wind plasma appears to be bounded by an exponential with an e‐folding distance of 1000 km.</jats:p>
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author Zong, Q.‐G., Fritz, T. A., Spence, H., Oksavik, K., Pu, Z.‐Y., Korth, A., Daly, P. W.
author_facet Zong, Q.‐G., Fritz, T. A., Spence, H., Oksavik, K., Pu, Z.‐Y., Korth, A., Daly, P. W., Zong, Q.‐G., Fritz, T. A., Spence, H., Oksavik, K., Pu, Z.‐Y., Korth, A., Daly, P. W.
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description <jats:p>In this paper we present new results using Cluster/Research with Adaptive Particle Imaging Detectors (RAPID) energetic particle observations to remotely sound the high‐latitude magnetopause in three dimensions. We demonstrate that energetic particle flux variations in the vicinity of the magnetopause (inside the magnetosphere) are mainly modulated by the absorbing magnetopause during quiet geomagnetic conditions. Less than two gyro radii from an absorbing boundary a trapped particle distribution becomes nongyrotropic, as particles start to encounter the boundary. Knowing the magnetic field and the particle mass and energy, the direction and distance to the magnetopause can be derived by examining the azimuthal distribution of locally mirroring particles. Combining observations from three nearby spacecraft gives a three‐dimensional, local picture of the magnetopause surface. We exploit anisotropic ion distributions to determine magnetopause distances, orientations, and structures in the interval from 1320 to 1420 UT on 14 January 2001 for the three Cluster spacecraft (Rumba, Samba, and Tango) located on the duskside (at ∼1700 MLT) high‐latitude region. The results clearly illustrate that the magnetopause ion sounding technique as proposed by <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0026"><jats:italic>Williams</jats:italic> [1979]</jats:ext-link>, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0006"><jats:italic>Fritz and Fahnenstiel</jats:italic> [1982]</jats:ext-link>, and <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0028"><jats:italic>Zong et al.</jats:italic> [2000]</jats:ext-link> can be used to remotely study the three‐dimensional orientation and location of the magnetopause surface and the gradient variation of the plasma parameters. Intercomparison between energetic particle sounding distance and simultaneous plasma and magnetic field measurements suggests that solar wind plasma can penetrate more than ≈1000 km deeper than the trapping boundary. The fluxes of different ion species are proportional to the distance from the magnetopause, with a correlation coefficient of 0.7 to 0.8. The energetic proton flux gradient as a function of distance from the magnetosphere is about 100 particles cm<jats:sup>−2</jats:sup> s<jats:sup>−1</jats:sup> sr<jats:sup>−1</jats:sup> per kilometer. In contrast, the solar wind plasma density is found to be inversely proportional to the distance. The solar wind plasma appears to be bounded by an exponential with an e‐folding distance of 1000 km.</jats:p>
doi_str_mv 10.1029/2003ja009929
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spelling Zong, Q.‐G. Fritz, T. A. Spence, H. Oksavik, K. Pu, Z.‐Y. Korth, A. Daly, P. W. 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/10.1029/2003ja009929 <jats:p>In this paper we present new results using Cluster/Research with Adaptive Particle Imaging Detectors (RAPID) energetic particle observations to remotely sound the high‐latitude magnetopause in three dimensions. We demonstrate that energetic particle flux variations in the vicinity of the magnetopause (inside the magnetosphere) are mainly modulated by the absorbing magnetopause during quiet geomagnetic conditions. Less than two gyro radii from an absorbing boundary a trapped particle distribution becomes nongyrotropic, as particles start to encounter the boundary. Knowing the magnetic field and the particle mass and energy, the direction and distance to the magnetopause can be derived by examining the azimuthal distribution of locally mirroring particles. Combining observations from three nearby spacecraft gives a three‐dimensional, local picture of the magnetopause surface. We exploit anisotropic ion distributions to determine magnetopause distances, orientations, and structures in the interval from 1320 to 1420 UT on 14 January 2001 for the three Cluster spacecraft (Rumba, Samba, and Tango) located on the duskside (at ∼1700 MLT) high‐latitude region. The results clearly illustrate that the magnetopause ion sounding technique as proposed by <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0026"><jats:italic>Williams</jats:italic> [1979]</jats:ext-link>, <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0006"><jats:italic>Fritz and Fahnenstiel</jats:italic> [1982]</jats:ext-link>, and <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#jgra17014-bib-0028"><jats:italic>Zong et al.</jats:italic> [2000]</jats:ext-link> can be used to remotely study the three‐dimensional orientation and location of the magnetopause surface and the gradient variation of the plasma parameters. Intercomparison between energetic particle sounding distance and simultaneous plasma and magnetic field measurements suggests that solar wind plasma can penetrate more than ≈1000 km deeper than the trapping boundary. The fluxes of different ion species are proportional to the distance from the magnetopause, with a correlation coefficient of 0.7 to 0.8. The energetic proton flux gradient as a function of distance from the magnetosphere is about 100 particles cm<jats:sup>−2</jats:sup> s<jats:sup>−1</jats:sup> sr<jats:sup>−1</jats:sup> per kilometer. In contrast, the solar wind plasma density is found to be inversely proportional to the distance. The solar wind plasma appears to be bounded by an exponential with an e‐folding distance of 1000 km.</jats:p> Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID Journal of Geophysical Research: Space Physics
spellingShingle Zong, Q.‐G., Fritz, T. A., Spence, H., Oksavik, K., Pu, Z.‐Y., Korth, A., Daly, P. W., Journal of Geophysical Research: Space Physics, Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID, 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 Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_full Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_fullStr Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_full_unstemmed Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_short Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
title_sort energetic particle sounding of the magnetopause: a contribution by cluster/rapid
title_unstemmed Energetic particle sounding of the magnetopause: A contribution by Cluster/RAPID
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/10.1029/2003ja009929