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Global Energetics of Solar Flares: IV. Coronal Mass Ejection Energetics

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arxiv 1605.04952 v1 pith:G5WVYICR submitted 2016-05-16 astro-ph.SR

classification astro-ph.SR
keywords dimmingenergymassmethodenergeticsenergiesevolutionflare
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abstract

This study entails the fourth part of a global flare energetics project, in which the mass $m_{\mathrm{cme}}$, kinetic energy $E_{\mathrm{kin}}$, and the gravitational potential energy $E_{\mathrm{grav}}$ of coronal mass ejections (CMEs) is measured in 399 M and X-class flare events observed during the first 3.5 yrs of the Solar Dynamics Observatory (SDO) mission, using a new method based on the EUV dimming effect. The EUV dimming is modeled in terms of a radial adiabatic expansion process, which is fitted to the observed evolution of the total emission measure of the CME source region. The model derives the evolution of the mean electron density, the emission measure, the bulk plasma expansion velocity, the mass, and the energy in the CME source region. The EUV dimming method is truly complementary to the Thomson scattering method in white light, which probes the CME evolution in the heliosphere at $r > 2 R_{\odot}$, while the EUV dimming method tracks the CME launch in the corona. We compare the CME parameters obtained in white light with the LASCO/C2 coronagraph with those obtained from EUV dimming with the Atmospheric Imaging Assembly (AIA) onboard SDO for all identical events in both data sets. We investigate correlations between CME parameters, the relative timing with flare parameters, frequency occurrence distributions, and the energy partition between magnetic, thermal, nonthermal, and CME energies. CME energies are found to be systematically lower than the dissipated magnetic energies, which is consistent with a magnetic origin of CMEs.

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  1. Coronal dimmings and what they tell us about solar and stellar coronal mass ejections

    astro-ph.SR 2025-05 conditional novelty 5.0 of 10

    A review of coronal dimmings that adds a new taxonomy based on the magnetic flux systems involved in eruptions, replacing the simple core/secondary morphology split.

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