Magnetic Decay Index Profile and Coronal Mass Ejection Speed
Bernhard Kliem, Georgios Chintzoglou, Tibor Török, Jie Zhang
TL;DR
The paper investigates how the ambient coronal magnetic-field profile, captured by the decay index $n(h)$, governs CME speeds through torus-instability-driven acceleration. It combines observational analysis of $n(h)$ profiles derived from potential-field extrapolations with a parametric MHD study of flux-rope eruptions in multipolar source regions to assess how dips in $n(h)$ affect acceleration. A striking result is that for very fast halo CMEs ($V_ ext{CME}\ge1500\,\mathrm{km\,s}^{-1}$), the slope of $n(h)$ above the TI onset height, $ig\langle n'(h)\big\bra_{\Delta h}$, correlates strongly with $V_ ext{CME}$, achieving $c\approx 0.81$ when outliers are excluded; dips in $n(h)$ can produce significant deceleration or confinement, reducing the correlation. These findings support TI as a principal driver of rapid CME acceleration and highlight the importance of coronal-field structure, particularly in multipolar regions, for forecasting CME speeds.
Abstract
We study the relationship between the speed of coronal mass ejections (CMEs) and the height profile of the ambient magnetic field, quantified by its decay index, n(h). Our sample is composed of 15 very fast CMEs (Vcme > 1500 km/s; all halo CMEs) and 22 halo CMEs below this speed limit from Solar Cycle 23. The very fast CMEs yield a high correlation of 0.81 between Vcme and the slope of n(h) in a height range above the onset height of the torus instability if one extremely fast outlier, which closely followed another very fast CME, is excluded. This is consistent with the hypothesis that the torus instability plays a decisive role in CME acceleration. The whole sample yields a weaker correlation, which is still significant if events with a broad torus-stable dip in n(h) are excluded. A parametric simulation study of flux-rope eruptions from quadrupolar and two-scale bipolar source regions confirms the decelerating effect of such dips. Very fast, moderate-velocity, and confined eruptions are found.
