Quasi-periodic emissions (15- 80 min ) from the poles of Jupiter as a principal source of the large-scale high-latitude magnetopause boundary layer of energetic particle

In this study, we concentrate on the examination of the quasi-periodic behavior of 0.5-1.6 MeV (∼40-400 keV) protons (electrons) and of relativistic (> 16 MeV) electrons, observed at Jupiter by two different experiments onboard Ulysses, the HI-SCALE and COSPIN, respectively, within the large-scal...

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Bibliographic Details
Main Authors: Karanikola, I., Athanasiou, M., Anagnostopoulos, G.C., Pavlos, G.P., Preka-Papadema, P.
Format: Article in Journal/Newspaper
Language:English
Published: 2004
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Online Access:https://pergamos.lib.uoa.gr/uoa/dl/object/uoadl:3017978
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Summary:In this study, we concentrate on the examination of the quasi-periodic behavior of 0.5-1.6 MeV (∼40-400 keV) protons (electrons) and of relativistic (> 16 MeV) electrons, observed at Jupiter by two different experiments onboard Ulysses, the HI-SCALE and COSPIN, respectively, within the large-scale south duskside magnetopause boundary layer (MPBL) of energetic particles, from ∼20:00 UT, day 41, to 12:00 UT, day 43. During those times, the observations confirm the transition of Ulysses to an important magnetospheric region with particle intensities comparable to the magnetodisk levels. A careful analysis of high time-resolution intensity, anisotropy and spectral measurements suggests the following: (1) The quasi-periodic ∼40 min (QP-40) energetic electron (> ∼40 keV) and proton (> ∼0.5 MeV) emissions from the south pole were a characteristic phenomenon in the south duskside MPBL; an almost continuous QP 40-min variation has been confirmed in energetic electron observations. (2) When the QP-40 modulation was not evident in energetic particle intensities, it was still detectable in spectral and anisotropy observations. (3) The QP-40 emission is a principal, but not the only periodic, energetic electron and proton emission; other periodicities (∼15, ∼20, ∼30, ∼50, ∼60, ∼80 min) were also significant in energetic particle spectral and anisotropy observations. We infer that QP-40 emissions along with other periodic emissions (∼15, ∼20, ∼30, ∼50, ∼60, ∼80 min) were the principal source of the large-scale high-latitude MPBL of energetic particles during Ulysses outbound pass of Jupiter. © 2003 Elsevier Ltd. All rights reserved.