Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum

The observational rate of mirror mode waves in Venus's magnetosheath for solar maximum conditions is studied and compared with previous results for solar minimum conditions. It is found that the number of mirror mode events is approximately 14 % higher for solar maximum than for solar minim...

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Main Authors: M. Volwerk, D. Schmid, B. T. Tsurutani, M. Delva, F. Plaschke, Y. Narita, T. Zhang, K.-H. Glassmeier
Format: Article
Language:English
Published: Copernicus Publications 2016-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/34/1099/2016/angeo-34-1099-2016.pdf
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author M. Volwerk
D. Schmid
D. Schmid
B. T. Tsurutani
M. Delva
F. Plaschke
Y. Narita
T. Zhang
T. Zhang
K.-H. Glassmeier
author_facet M. Volwerk
D. Schmid
D. Schmid
B. T. Tsurutani
M. Delva
F. Plaschke
Y. Narita
T. Zhang
T. Zhang
K.-H. Glassmeier
author_sort M. Volwerk
collection DOAJ
description The observational rate of mirror mode waves in Venus's magnetosheath for solar maximum conditions is studied and compared with previous results for solar minimum conditions. It is found that the number of mirror mode events is approximately 14 % higher for solar maximum than for solar minimum. A possible cause is the increase in solar UV radiation, ionizing more neutrals from Venus's exosphere and the outward displacement of the bow shock during solar maximum. Also, the solar wind properties (speed, density) differ for solar minimum and maximum. The maximum observational rate, however, over Venus's magnetosheath remains almost the same, with only differences in the distribution along the flow line. This may be caused by the interplay of a decreasing solar wind density and a slightly higher solar wind velocity for this solar maximum. The distribution of strengths of the mirror mode waves is shown to be exponentially falling off, with (almost) the same coefficient for solar maximum and minimum. The plasma conditions in Venus's magnetosheath are different for solar minimum as compared to solar maximum. For solar minimum, mirror mode waves are created directly behind where the bow shock will decay, whereas for solar maximum all created mirror modes can grow.
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spelling doaj.art-caf0a032ed184c8badf16c198fae13262022-12-22T03:56:35ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762016-11-01341099110810.5194/angeo-34-1099-2016Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximumM. Volwerk0D. Schmid1D. Schmid2B. T. Tsurutani3M. Delva4F. Plaschke5Y. Narita6T. Zhang7T. Zhang8K.-H. Glassmeier9Space Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaUniversity of Graz, NAWI Graz, Graz, AustriaCalifornia Institute of Technology, Pasadena, California, USASpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaSpace Research Institute, Austrian Academy of Sciences, Graz, AustriaCAS Key Laboratory of Geospace Environment, University of Science and Technology of China, Hefei, ChinaInstitute for Geophysics and Extraterrestrial Physics, TU Braunschweig, Braunschweig, GermanyThe observational rate of mirror mode waves in Venus's magnetosheath for solar maximum conditions is studied and compared with previous results for solar minimum conditions. It is found that the number of mirror mode events is approximately 14 % higher for solar maximum than for solar minimum. A possible cause is the increase in solar UV radiation, ionizing more neutrals from Venus's exosphere and the outward displacement of the bow shock during solar maximum. Also, the solar wind properties (speed, density) differ for solar minimum and maximum. The maximum observational rate, however, over Venus's magnetosheath remains almost the same, with only differences in the distribution along the flow line. This may be caused by the interplay of a decreasing solar wind density and a slightly higher solar wind velocity for this solar maximum. The distribution of strengths of the mirror mode waves is shown to be exponentially falling off, with (almost) the same coefficient for solar maximum and minimum. The plasma conditions in Venus's magnetosheath are different for solar minimum as compared to solar maximum. For solar minimum, mirror mode waves are created directly behind where the bow shock will decay, whereas for solar maximum all created mirror modes can grow.https://www.ann-geophys.net/34/1099/2016/angeo-34-1099-2016.pdf
spellingShingle M. Volwerk
D. Schmid
D. Schmid
B. T. Tsurutani
M. Delva
F. Plaschke
Y. Narita
T. Zhang
T. Zhang
K.-H. Glassmeier
Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
Annales Geophysicae
title Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
title_full Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
title_fullStr Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
title_full_unstemmed Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
title_short Mirror mode waves in Venus's magnetosheath: solar minimum vs. solar maximum
title_sort mirror mode waves in venus s magnetosheath solar minimum vs solar maximum
url https://www.ann-geophys.net/34/1099/2016/angeo-34-1099-2016.pdf
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