author_facet Boardsen, S. A.
Jian, L. K.
Raines, J. L.
Gershman, D. J.
Zurbuchen, T. H.
Roberts, D. A.
Korth, H.
Boardsen, S. A.
Jian, L. K.
Raines, J. L.
Gershman, D. J.
Zurbuchen, T. H.
Roberts, D. A.
Korth, H.
author Boardsen, S. A.
Jian, L. K.
Raines, J. L.
Gershman, D. J.
Zurbuchen, T. H.
Roberts, D. A.
Korth, H.
spellingShingle Boardsen, S. A.
Jian, L. K.
Raines, J. L.
Gershman, D. J.
Zurbuchen, T. H.
Roberts, D. A.
Korth, H.
Journal of Geophysical Research: Space Physics
MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
Space and Planetary Science
Geophysics
author_sort boardsen, s. a.
spelling Boardsen, S. A. Jian, L. K. Raines, J. L. Gershman, D. J. Zurbuchen, T. H. Roberts, D. A. Korth, H. 2169-9380 2169-9402 American Geophysical Union (AGU) Space and Planetary Science Geophysics http://dx.doi.org/10.1002/2015ja021506 <jats:title>Abstract</jats:title><jats:p>MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) magnetometer data was surveyed between 0.3 and 0.7 AU from 6 June 2007 to 23 March 2011 for low‐frequency wave (LFW) storms, when the magnetometer was sampling at a rate of at least 2 s<jats:sup>−1</jats:sup>. A total of 12,197 LFW events were identified, of which 5506 lasted 10 min or longer. The events have a high degree of polarization, are circularly polarized, with wave vectors nearly aligned or antialigned with the interplanetary magnetic field (IMF) at frequencies in the vicinity of the proton cyclotron frequency. These events are observed about 6% of the time, preferentially associated with radially directed inward or outward IMF. Their occurrence rate and median duration do not change much with <jats:italic>R</jats:italic>, where <jats:italic>R</jats:italic> is the heliocentric radial distance. For a narrow‐frequency window in the solar wind frame, left‐handed storms in the spacecraft frame have a power drop off that is roughly proportional to <jats:italic>R</jats:italic><jats:sup>−3</jats:sup> which is consistent with a source close the Sun, while right‐handed storms have a power drop off roughly proportional <jats:italic>R</jats:italic><jats:sup>−1</jats:sup> which is not consistent with a source close to the Sun. The power in the left‐handed LFW storms is on average greater than the right‐handed ones by a factor of 3. In the solar wind frame, the wave frequency decreases from 0.13 to 0.04 Hz moving from 0.3 to 0.7 AU, but the frequency normalized by the local proton cyclotron frequency does not change much with the running median varying from 0.35 to 0.5. The normalized frequency band widths of the wave power spectra increase slightly with <jats:italic>R</jats:italic>, possibly associated with energy dissipation.</jats:p> MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU Journal of Geophysical Research: Space Physics
doi_str_mv 10.1002/2015ja021506
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Geologie und Paläontologie
Geographie
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imprint American Geophysical Union (AGU), 2015
imprint_str_mv American Geophysical Union (AGU), 2015
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match_str boardsen2015messengersurveyofinsitulowfrequencywavestormsbetween03and07au
publishDateSort 2015
publisher American Geophysical Union (AGU)
recordtype ai
record_format ai
series Journal of Geophysical Research: Space Physics
source_id 49
title MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_unstemmed MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_full MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_fullStr MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_full_unstemmed MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_short MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_sort messenger survey of in situ low frequency wave storms between 0.3 and 0.7 au
topic Space and Planetary Science
Geophysics
url http://dx.doi.org/10.1002/2015ja021506
publishDate 2015
physical
description <jats:title>Abstract</jats:title><jats:p>MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) magnetometer data was surveyed between 0.3 and 0.7 AU from 6 June 2007 to 23 March 2011 for low‐frequency wave (LFW) storms, when the magnetometer was sampling at a rate of at least 2 s<jats:sup>−1</jats:sup>. A total of 12,197 LFW events were identified, of which 5506 lasted 10 min or longer. The events have a high degree of polarization, are circularly polarized, with wave vectors nearly aligned or antialigned with the interplanetary magnetic field (IMF) at frequencies in the vicinity of the proton cyclotron frequency. These events are observed about 6% of the time, preferentially associated with radially directed inward or outward IMF. Their occurrence rate and median duration do not change much with <jats:italic>R</jats:italic>, where <jats:italic>R</jats:italic> is the heliocentric radial distance. For a narrow‐frequency window in the solar wind frame, left‐handed storms in the spacecraft frame have a power drop off that is roughly proportional to <jats:italic>R</jats:italic><jats:sup>−3</jats:sup> which is consistent with a source close the Sun, while right‐handed storms have a power drop off roughly proportional <jats:italic>R</jats:italic><jats:sup>−1</jats:sup> which is not consistent with a source close to the Sun. The power in the left‐handed LFW storms is on average greater than the right‐handed ones by a factor of 3. In the solar wind frame, the wave frequency decreases from 0.13 to 0.04 Hz moving from 0.3 to 0.7 AU, but the frequency normalized by the local proton cyclotron frequency does not change much with the running median varying from 0.35 to 0.5. The normalized frequency band widths of the wave power spectra increase slightly with <jats:italic>R</jats:italic>, possibly associated with energy dissipation.</jats:p>
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author Boardsen, S. A., Jian, L. K., Raines, J. L., Gershman, D. J., Zurbuchen, T. H., Roberts, D. A., Korth, H.
author_facet Boardsen, S. A., Jian, L. K., Raines, J. L., Gershman, D. J., Zurbuchen, T. H., Roberts, D. A., Korth, H., Boardsen, S. A., Jian, L. K., Raines, J. L., Gershman, D. J., Zurbuchen, T. H., Roberts, D. A., Korth, H.
author_sort boardsen, s. a.
container_issue 12
container_start_page 0
container_title Journal of Geophysical Research: Space Physics
container_volume 120
description <jats:title>Abstract</jats:title><jats:p>MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) magnetometer data was surveyed between 0.3 and 0.7 AU from 6 June 2007 to 23 March 2011 for low‐frequency wave (LFW) storms, when the magnetometer was sampling at a rate of at least 2 s<jats:sup>−1</jats:sup>. A total of 12,197 LFW events were identified, of which 5506 lasted 10 min or longer. The events have a high degree of polarization, are circularly polarized, with wave vectors nearly aligned or antialigned with the interplanetary magnetic field (IMF) at frequencies in the vicinity of the proton cyclotron frequency. These events are observed about 6% of the time, preferentially associated with radially directed inward or outward IMF. Their occurrence rate and median duration do not change much with <jats:italic>R</jats:italic>, where <jats:italic>R</jats:italic> is the heliocentric radial distance. For a narrow‐frequency window in the solar wind frame, left‐handed storms in the spacecraft frame have a power drop off that is roughly proportional to <jats:italic>R</jats:italic><jats:sup>−3</jats:sup> which is consistent with a source close the Sun, while right‐handed storms have a power drop off roughly proportional <jats:italic>R</jats:italic><jats:sup>−1</jats:sup> which is not consistent with a source close to the Sun. The power in the left‐handed LFW storms is on average greater than the right‐handed ones by a factor of 3. In the solar wind frame, the wave frequency decreases from 0.13 to 0.04 Hz moving from 0.3 to 0.7 AU, but the frequency normalized by the local proton cyclotron frequency does not change much with the running median varying from 0.35 to 0.5. The normalized frequency band widths of the wave power spectra increase slightly with <jats:italic>R</jats:italic>, possibly associated with energy dissipation.</jats:p>
doi_str_mv 10.1002/2015ja021506
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imprint American Geophysical Union (AGU), 2015
imprint_str_mv American Geophysical Union (AGU), 2015
institution DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229
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match_str boardsen2015messengersurveyofinsitulowfrequencywavestormsbetween03and07au
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physical
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record_format ai
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spelling Boardsen, S. A. Jian, L. K. Raines, J. L. Gershman, D. J. Zurbuchen, T. H. Roberts, D. A. Korth, H. 2169-9380 2169-9402 American Geophysical Union (AGU) Space and Planetary Science Geophysics http://dx.doi.org/10.1002/2015ja021506 <jats:title>Abstract</jats:title><jats:p>MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) magnetometer data was surveyed between 0.3 and 0.7 AU from 6 June 2007 to 23 March 2011 for low‐frequency wave (LFW) storms, when the magnetometer was sampling at a rate of at least 2 s<jats:sup>−1</jats:sup>. A total of 12,197 LFW events were identified, of which 5506 lasted 10 min or longer. The events have a high degree of polarization, are circularly polarized, with wave vectors nearly aligned or antialigned with the interplanetary magnetic field (IMF) at frequencies in the vicinity of the proton cyclotron frequency. These events are observed about 6% of the time, preferentially associated with radially directed inward or outward IMF. Their occurrence rate and median duration do not change much with <jats:italic>R</jats:italic>, where <jats:italic>R</jats:italic> is the heliocentric radial distance. For a narrow‐frequency window in the solar wind frame, left‐handed storms in the spacecraft frame have a power drop off that is roughly proportional to <jats:italic>R</jats:italic><jats:sup>−3</jats:sup> which is consistent with a source close the Sun, while right‐handed storms have a power drop off roughly proportional <jats:italic>R</jats:italic><jats:sup>−1</jats:sup> which is not consistent with a source close to the Sun. The power in the left‐handed LFW storms is on average greater than the right‐handed ones by a factor of 3. In the solar wind frame, the wave frequency decreases from 0.13 to 0.04 Hz moving from 0.3 to 0.7 AU, but the frequency normalized by the local proton cyclotron frequency does not change much with the running median varying from 0.35 to 0.5. The normalized frequency band widths of the wave power spectra increase slightly with <jats:italic>R</jats:italic>, possibly associated with energy dissipation.</jats:p> MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU Journal of Geophysical Research: Space Physics
spellingShingle Boardsen, S. A., Jian, L. K., Raines, J. L., Gershman, D. J., Zurbuchen, T. H., Roberts, D. A., Korth, H., Journal of Geophysical Research: Space Physics, MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU, Space and Planetary Science, Geophysics
title MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_full MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_fullStr MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_full_unstemmed MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_short MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
title_sort messenger survey of in situ low frequency wave storms between 0.3 and 0.7 au
title_unstemmed MESSENGER survey of in situ low frequency wave storms between 0.3 and 0.7 AU
topic Space and Planetary Science, Geophysics
url http://dx.doi.org/10.1002/2015ja021506