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Fluctuations of Solar Wind Parameters During Polar Reversal

Received: 9 April 2015    Accepted: 1 May 2015    Published: 19 May 2015
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Abstract

Around the time of polarity reversal in 2000 – 2001, the solar wind plasma parameters and interplanetary magnetic field fluctuations are studied for an interval of time that corresponds to Ulysses in-situ measurements of high-latitude heliospheric magnetic field. This study has been done by investigating solar wind speed, density, temperature and solar magnetic field using Ulysses magnetometer and SWOOPS instrument. The sun's magnetic field reverses polarity approximately in every 11 year and it creates a peak in each solar cycle. This study gives a brief understanding of solar wind parameters in the heliosphere during polar reversal in solar cycle 23. The solar magnetic field completely reorganizes during the polar reversal phase, hence the distribution of solar wind parameters changes accordingly. By studying the variation of solar wind parameters, it is possible to understand the polar reversal phenomenon. The photospheric polarity reversal is completed in more active Northern Hemisphere in late 2000 and then in the Southern Hemisphere in 2001. The reversal of the magnetic field at the solar wind source surface is inferred to have occurred between late 2000 and 2001, with the most likely time of reversal being early within that period.

Published in American Journal of Astronomy and Astrophysics (Volume 3, Issue 3)
DOI 10.11648/j.ajaa.20150303.15
Page(s) 56-62
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Heliosphere, Interplanetary Magnetic Field, Solar Wind

References
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    Iren Sobia, Bidhu S. S., Dickson Benjamin. (2015). Fluctuations of Solar Wind Parameters During Polar Reversal. American Journal of Astronomy and Astrophysics, 3(3), 56-62. https://doi.org/10.11648/j.ajaa.20150303.15

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    ACS Style

    Iren Sobia; Bidhu S. S.; Dickson Benjamin. Fluctuations of Solar Wind Parameters During Polar Reversal. Am. J. Astron. Astrophys. 2015, 3(3), 56-62. doi: 10.11648/j.ajaa.20150303.15

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    AMA Style

    Iren Sobia, Bidhu S. S., Dickson Benjamin. Fluctuations of Solar Wind Parameters During Polar Reversal. Am J Astron Astrophys. 2015;3(3):56-62. doi: 10.11648/j.ajaa.20150303.15

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  • @article{10.11648/j.ajaa.20150303.15,
      author = {Iren Sobia and Bidhu S. S. and Dickson Benjamin},
      title = {Fluctuations of Solar Wind Parameters During Polar Reversal},
      journal = {American Journal of Astronomy and Astrophysics},
      volume = {3},
      number = {3},
      pages = {56-62},
      doi = {10.11648/j.ajaa.20150303.15},
      url = {https://doi.org/10.11648/j.ajaa.20150303.15},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajaa.20150303.15},
      abstract = {Around the time of polarity reversal in 2000 – 2001, the solar wind plasma parameters and interplanetary magnetic field fluctuations are studied for an interval of time that corresponds to Ulysses in-situ measurements of high-latitude heliospheric magnetic field. This study has been done by investigating solar wind speed, density, temperature and solar magnetic field using Ulysses magnetometer and SWOOPS instrument. The sun's magnetic field reverses polarity approximately in every 11 year and it creates a peak in each solar cycle. This study gives a brief understanding of solar wind parameters in the heliosphere during polar reversal in solar cycle 23. The solar magnetic field completely reorganizes during the polar reversal phase, hence the distribution of solar wind parameters changes accordingly. By studying the variation of solar wind parameters, it is possible to understand the polar reversal phenomenon. The photospheric polarity reversal is completed in more active Northern Hemisphere in late 2000 and then in the Southern Hemisphere in 2001. The reversal of the magnetic field at the solar wind source surface is inferred to have occurred between late 2000 and 2001, with the most likely time of reversal being early within that period.},
     year = {2015}
    }
    

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  • TY  - JOUR
    T1  - Fluctuations of Solar Wind Parameters During Polar Reversal
    AU  - Iren Sobia
    AU  - Bidhu S. S.
    AU  - Dickson Benjamin
    Y1  - 2015/05/19
    PY  - 2015
    N1  - https://doi.org/10.11648/j.ajaa.20150303.15
    DO  - 10.11648/j.ajaa.20150303.15
    T2  - American Journal of Astronomy and Astrophysics
    JF  - American Journal of Astronomy and Astrophysics
    JO  - American Journal of Astronomy and Astrophysics
    SP  - 56
    EP  - 62
    PB  - Science Publishing Group
    SN  - 2376-4686
    UR  - https://doi.org/10.11648/j.ajaa.20150303.15
    AB  - Around the time of polarity reversal in 2000 – 2001, the solar wind plasma parameters and interplanetary magnetic field fluctuations are studied for an interval of time that corresponds to Ulysses in-situ measurements of high-latitude heliospheric magnetic field. This study has been done by investigating solar wind speed, density, temperature and solar magnetic field using Ulysses magnetometer and SWOOPS instrument. The sun's magnetic field reverses polarity approximately in every 11 year and it creates a peak in each solar cycle. This study gives a brief understanding of solar wind parameters in the heliosphere during polar reversal in solar cycle 23. The solar magnetic field completely reorganizes during the polar reversal phase, hence the distribution of solar wind parameters changes accordingly. By studying the variation of solar wind parameters, it is possible to understand the polar reversal phenomenon. The photospheric polarity reversal is completed in more active Northern Hemisphere in late 2000 and then in the Southern Hemisphere in 2001. The reversal of the magnetic field at the solar wind source surface is inferred to have occurred between late 2000 and 2001, with the most likely time of reversal being early within that period.
    VL  - 3
    IS  - 3
    ER  - 

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Author Information
  • Department of Physics, Nesamony Memorial Christian College, Marthandam, Tamil Nadu, India

  • Department of Physics, Nesamony Memorial Christian College, Marthandam, Tamil Nadu, India

  • Department of Physics, Nesamony Memorial Christian College, Marthandam, Tamil Nadu, India

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