Geomagnetically Induced Currents Caused by Interplanetary Shocks With Different Impact Angles and Speeds

  • D. M. Oliveira
    Goddard Planetary Heliophysics Institute University of Maryland, Baltimore County Baltimore MD USA
  • D. Arel
    Department of Physics and EOS Space Science Center University of New Hampshire Durham NH USA
  • J. Raeder
    Department of Physics and EOS Space Science Center University of New Hampshire Durham NH USA
  • E. Zesta
    NASA Goddard Space Flight Center Greenbelt MD USA
  • C. M. Ngwira
    NASA Goddard Space Flight Center Greenbelt MD USA
  • B. A. Carter
    SPACE Research Centre RMIT University Melbourne Victoria Australia
  • E. Yizengaw
    Institute for Scientific Research Boston College Boston MA USA
  • A. J. Halford
    The Aerospace Corporation Chantilly VA USA
  • B. T. Tsurutani
    Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
  • J. W. Gjerloev
    The Johns Hopkins University Applied Physics Laboratory Laurel MD USA

書誌事項

公開日
2018-06
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2018sw001880
公開者
American Geophysical Union (AGU)

この論文をさがす

説明

<jats:title>Abstract</jats:title><jats:p>The occurrence of geomagnetically induced currents (GICs) poses serious threats to modern technological infrastructure. Large GICs result from sharp variations of the geomagnetic field (d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic>) caused by changes of large‐scale magnetospheric and ionospheric currents. Intense d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> perturbations are known to occur often in high‐latitude regions as a result of storm time substorms. Magnetospheric compressions usually caused by interplanetary shocks increase the magnetopause current leading to d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> perturbations more evident in midlatitude to low‐latitude regions, while they increase the equatorial electrojet current leading to d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> perturbations in dayside equatorial regions. We investigate the effects of shock impact angles and speeds on the subsequent d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> perturbations with a database of 547 shocks observed at the L1 point. By adopting the threshold of d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> = 100 nT/min, identified as a risk factor to power systems, we find that d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> generally surpasses this threshold when following impacts of high‐speed and nearly frontal shocks in dayside high‐latitude locations. The same trend occurs at lower latitudes and for all nightside events but with fewer high‐risk events. Particularly, we found nine events in equatorial locations with d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> > 100 nT/min. All events were caused by high‐speed and nearly frontal shock impacts and were observed by stations located around noon local time. These high‐risk perturbations were caused by sudden strong and symmetric magnetospheric compressions, more effectively intensifying the equatorial electrojet current, leading to sharp d<jats:italic>B</jats:italic>/d<jats:italic>t</jats:italic> perturbations. We suggest that these results may provide insights for GIC forecasting aiming at preventing degradation of power systems due to GICs.</jats:p>

収録刊行物

  • Space Weather

    Space Weather 16 (6), 636-647, 2018-06

    American Geophysical Union (AGU)

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