Dependence of great geomagnetic storm intensity (SYM-H-200 nT) on associated solar wind parameters
arXiv:2009.05971 · doi:10.1007/s11207-021-01816-2
Abstract
We use SYM-H to capture the variation in the SYM-H index during the main phase of a geomagnetic storm. We define great geomagnetic storms as those with SYM-H -200 nT. After analyzing the data that were not obscured by solar winds, we determined that 11 such storms occurred during solar cycle 23. We calculated time integrals for the southward interplanetary magnetic field component I(B), the solar wind electric field I(E), and a combination of E and the solar wind dynamic pressure I(Q) during the main phase of a great geomagnetic storm. The strength of the correlation coefficient (CC) between SYM-H and each of the three integrals I(B) (CC = 0.74), I(E) (CC = 0.85), and I(Q) (CC = 0.94) suggests that Q, which encompasses both the solar wind electric field and the solar wind dynamic pressure, is the main driving factor that determines the intensity of a great geomagnetic storm. The results also suggest that the impact of B on the great geomagnetic storm intensity is much more significant than that of the solar wind speed and the dynamic pressure during the main phase of associated great geomagnetic storm. How to estimate the intensity of an extreme geomagnetic storm based on solar wind parameters is also discussed.
3 figures
References in corpus (4)
- Observations of an extreme storm in interplanetary space caused by successive coronal mass ejections
- Dependence of Intensities of Major Geomagnetic Storms (Dst -100 nT) on Associated Solar Wind Parameters
- Characteristics and Importance of "ICME-in-Sheath" Phenomenon and Upper Limit for Geomagnetic Storm Activity
- Extreme space weather events caused by super active regions during solar cycles 21-24
Cited by in corpus (4)
- The Sun and Space Weather
- What is Unusual about the Third Largest Geomagnetic Storm of Solar Cycle 24?
- Can we estimate the intensities of great geomagnetic storms(SYM-H200 nT) by Burton equation or by O'Brien and McPherron equation?
- The Stochastic-Dissipative Störmer Problem-Trajectories and Radiation Patterns