Finding the critical decay index in solar prominence eruptions
N. Vasantharaju, P. Vemareddy, B. Ravindra, and V. H. Doddamani

TL;DR
This study determines the critical decay index for prominence eruptions using multi-perspective observations, revealing a range of 0.8-1.3 and highlighting the dominant role of magnetic reconnection over torus-instability in flare-associated eruptions.
Contribution
It provides the first observational determination of the critical decay index for prominence eruptions, refining the understanding of eruption onset conditions.
Findings
Critical decay index varies from 0.8 to 1.3.
Flare-associated eruptions show significantly higher acceleration.
Magnetic reconnection dominates over torus-instability in eruption acceleration.
Abstract
The background field is assumed to play prime role in the erupting structures like prominences. In the flux rope models, the critical decay index () is a measure of the rate at which background field intensity decreases with height over the flux rope or erupting structure. In the real observations, the critical height of the background field is unknown, so a typical value of is adopted from the numerical studies. In this study, we determined the of 10 prominence eruptions (PEs). The prominence height in 3D is derived from two-perspective observations of \textit{Solar Dynamics Observatory} and \textit{Solar TErrestrial RElations Observatory}. Synoptic maps of photospheric radial magnetic field are used to construct the background field in the corona. During the eruption, the height-time curve of the sample events exhibits the slow and fast-rise phases and is fitted…
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