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However, the correlation coefficients between the trough position and other related main phase parameters are very low.
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In quiet conditions, the difference between the trough positions of the Northern Hemisphere and that of the Southern Hemisphere is mainly due to the longitudinal difference.
Figure 7 shows the relationship between the minimum latitude of the trough position and the storm magnitude.
Fig. 7 Relationship between the minimum latitude of the trough position and the storm magnitude.
We also calculated the correlation between the minimum latitude of the trough position and the storm magnitude as well as other related main phase parameters during all storms.
Because ΔDst correlates with Dstmin, the correlation with P value <0.001 between the minimum latitude of the trough position and ΔDst are also statistically significant.
However, the correlation between the minimum latitude of the trough position and Dstmax and ΔT is weak (correlation coefficient <0.3) and not significant (P value >0.1).
It is evident that there is a strong (correlation coefficients >0.8) and significant (P value <0.0001) correlation between the minimum latitude of the trough position and the Dstmin.
The correlation coefficients and P values are calculated to determine the relationship between the minimum latitude of the trough position and the storm magnitude as well as other related main phase parameters during all storms.
Therefore, the local time distribution of the trough position is small and the local time effect of the trough position can be neglected.
Therefore, the trough position follows a similar variation throughout the storm sequence regardless of hemispheres.
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