4.7 Article

A comptonized fireball bubble: physical origin of magnetar giant flares

Journal

MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 520, Issue 4, Pages 6195-6213

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/mnras/stad443

Keywords

stars: magnetars; gamma-ray bursts

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Magnetar giant flares (MGFs) are believed to contribute to some short gamma-ray bursts (GRBs). The recent discovery of short GRB 200415A in NGC 253 has established a connection between these two phenomena. The paper proposes a new model for MGFs, which involves an expanding fireball Comptonized by the relativistic magnetar wind at the photosphere radius. By fitting the observational spectra of GRB 200415A, the model predictions are found to be consistent with the observations.
Magnetar giant flares (MGFs) have been long proposed to contribute at least a subsample of the observed short gamma-ray bursts (GRBs). The recent discovery of the short GRB 200415A in the nearby galaxy NGC 253 established a textbook-version connection between these two phenomena. Unlike previous observations of the Galactic MGFs, the unsaturated instrument spectra of GRB 200415A provide for the first time an opportunity to test the theoretical models with the observed gamma-ray photons. This paper proposed a new readily fit-able model for the MGFs, which invokes an expanding fireball Comptonized by the relativistic magnetar wind at photosphere radius. In this model, a large amount of energy is released from the magnetar crust due to the magnetic reconnection or the starquakes of the star surface and is injected into confined field lines, forming a trapped fireball bubble. After breaking through the shackles and expanding to the photospheric radius, the thermal photons of the fireball are eventually Comptonized by the relativistic e(+/-) pairs in the magnetar wind region, which produces additional higher-energy gamma-ray emission. The model predicts a modified thermal-like spectrum characterized by a low-energy component in the Rayleigh-Jeans regime, a smooth component affected by coherent Compton scattering in the intermediate energy range, and a high-energy tail due to the inverse Compton process. By performing a Monte-Carlo fit to the observational spectra of GRB 200415A, we found that the observation of the burst is entirely consistent with our model predictions.

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