• Title/Summary/Keyword: solar wind dynamic pressure enhancements

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Statistical study of solar wind dynamic pressure enhancements during geomagnetic storms: Preliminary results

  • Baek, Ji-Hye;Lee, Dae-Young
    • Bulletin of the Korean Space Science Society
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    • 2004.04a
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    • pp.93-93
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    • 2004
  • We have examined the solar wind dynamic pressure enhancements during geomagnetic storm main phase. The Dst index has been used to identify more than 100 geomagnetic storms which occurred in the time interval of 1997 to 2001. We have selected only the events having the minimum Dst value less than -50 nT. In order to identify the pressure impact, we have looked at the low latitude ground H data as well as the solar wind pressure data themselves. (omitted)

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Statistical Characteristics of Solar Wind Dynamic Pressure Enhancements During Geomagnetic Storms

  • Choi, C.R.;Kim, K.C.;Lee, D.Y.;Kim, J.H.;Lee, E.
    • Journal of Astronomy and Space Sciences
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    • v.25 no.2
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    • pp.113-128
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    • 2008
  • Solar wind dynamic pressure enhancements are known to cause various types of disturbances to the magnetosphere. In particular, dynamic pressure enhancements may affect the evolution of magnetic storms when they occur during storm times. In this paper, we have investigated the statistical significance and features of dynamic pressure enhancements during magnetic storm times. For the investigation, we have used a total of 91 geomagnetic storms for 2001-2003, for which the Dst minimum $(Dst_{min})$ is below -50 nT. Also, we have imposed a set of selection criteria for a pressure enhancement to be considered an event: The main selection criterion is that the pressure increases by ${\geq}50%\;or\;{\geq}3nPa$ within 30 min and remains to be elevated for 10 min or longer. For our statistical analysis, we define the storm time to be the interval from the main Dst decrease, through $Dst_{min}$, to the point where the Dst index recovers by 50%. Our main results are summarized as follows. $(i){\sim}$ 81% of the studied storms indicate at least one event of pressure enhancements. When averaged over all the 91 storms, the occurrence rate is ${\sim}$ 4.5 pressure enhancement events per storm and ${\sim}$ 0.15 pressure enhancement events per hour. (ii) The occurrence rate of the pressure enhancements is about three times higher for CME-driven storm times than for CIR-driven storm times. (iii) Only 21.1% of the pressure enhancements show a clear association with an interplanetary shock. (iv) A large number of the pressure enhancement events are accompanied with a simultaneous change of IMF $B_y$ and/or $B_z$: For example, 73.5% of the pressure enhancement events are associated with an IMF change of either $|{\Delta}B_z|>2nT\;or\;|{\Delta}B_y|>2nT$. This last finding suggests that one should consider possible interplay effects between the simultaneous pressure and IMF changes in many situations.

Geosynchronous Relativistic Electron Events Associated with High-Speed Solar Wind Streams in 2006 (2006년 발생한 고속 태양풍과 관련된 정지궤도에서의 상대론적 전자 증가 이벤트)

  • Lee, Sung-Eun;Hwang, Jung-A;Lee, Jae-Jin;Cho, Kyung-Suk;Kim, Khan-Hyuk;Yi, Yu
    • Journal of Astronomy and Space Sciences
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    • v.26 no.4
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    • pp.439-450
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    • 2009
  • Recurrent enhancements of relativistic electron events at geosynchronous orbit (GREEs) were observed in 2006. These GREE enhancements were associated with high-speed solar wind streams coming from the same coronal hole. For the first six months of 2006, the occurrence of GREEs has 27 day periodicity and the GREEs were enhanced with various flux levels. Several factors have been studied to be related to GREEs: (1) High speed stream, (2) Pc5 ULF wave activity, (3) Southward IMF Bz, (4) substorm occurrence, (5) Whistler mode chorus wave, and (6) Dynamic pressure. In this paper, we have examined the effectiveness about those parameters in selected periods.