1992Geophysical Research LettersRequires access

ISEE 3 plasmoid and TCR observations during an extended interval of substorm activity

J. A. Slavin, Mark F. Smith, E. L. Mazur, D. N. Baker, T. Iyemori, H. J. Singer, E. W. Greenstadt

Open publisher page 68 citations

Abstract

On April 9–11, 1983, the ISEE 3 spacecraft was continuously located within the Earth's magnetotail for more than 36 hours at downstream distances of X= −76 to −80 Re. During this span of time, 12 major intervals of substorm activity were observed in the AL index with good ISEE 3 telemetry coverage for 11 of them. In addition, there were two small substorms outside of these intervals, both with complete observations in the distant tail. This unusual ISEE 3 data set provides a unique opportunity to test the predictions of the near‐Earth neutral line model. In particular, we examine the hypothesis that energy stored in the tail lobes during the growth phase is later dissipated, in part, through the release of one or more plasmoids following expansion phase onset. Clear growth phase enhancements in the lobe magnetic field intensity preceded the onsets of nine of the substorms. Plasmoids, or their lobe signatures, traveling compression regions (TCRs), were observed at ISEE 3 in association with all 11 of the major substorm intervals for which there were ISEE observations as well as for the two small substorms. No plasmoids or TCRs were observed in the absence of substorm activity. If these ISEE 3 observations are representative, then the release of plasmoids down the tail may be a feature common to all substorms.

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What this paper is about

On April 9–11, 1983, the ISEE 3 spacecraft was continuously located within the Earth's magnetotail for more than 36 hours at downstream distances of X= −76 to −80 Re. During this span of time, 12 major intervals of substorm activity were observed in the AL index with good ISEE 3 telemetry coverage for 11 of them. In addition, there were two small substorms outside of these intervals, both with complete observations in the distant tail. This unusual ISEE 3 data set provides a unique opportunity to test the predictions of the near‐Earth neutral line model. In particular, we examine the hypothesis that energy stored in the tail lobes during the growth phase is later dissipated, in part, through the release of one or more plasmoids following expansion phase onset. Clear growth phase enhancements in the lobe magnetic field intensity preceded the onsets of nine of the substorms. Plasmoids, or their lobe signatures, traveling compression regions (TCRs), were observed at ISEE 3 in association with all 11 of the major substorm intervals for which there were ISEE observations as well as for the two small substorms. No plasmoids or TCRs were observed in the absence of substorm activity. If these ISEE 3 observations are representative, then the release of plasmoids down the tail may be a feature common to all substorms.

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Available abstract

On April 9–11, 1983, the ISEE 3 spacecraft was continuously located within the Earth's magnetotail for more than 36 hours at downstream distances of X= −76 to −80 Re. During this span of time, 12 major intervals of substorm activity were observed in the AL index with good ISEE 3 telemetry coverage for 11 of them. In addition, there were two small substorms outside of these intervals, both with complete observations in the distant tail. This unusual ISEE 3 data set provides a unique opportunity to test the predictions of the near‐Earth neutral line model. In particular, we examine the hypothesis that energy stored in the tail lobes during the growth phase is later dissipated, in part, through the release of one or more plasmoids following expansion phase onset. Clear growth phase enhancements in the lobe magnetic field intensity preceded the onsets of nine of the substorms. Plasmoids, or their lobe signatures, traveling compression regions (TCRs), were observed at ISEE 3 in association with all 11 of the major substorm intervals for which there were ISEE observations as well as for the two small substorms. No plasmoids or TCRs were observed in the absence of substorm activity. If these ISEE 3 observations are representative, then the release of plasmoids down the tail may be a feature common to all substorms.

Key concepts: Substorm, Plasmoid, Physics, Geophysics, Astrophysics, Magnetic reconnection, Magnetosphere, Plasma

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