Comparative study of the inial spikes of SGR giant flares in 1998 and 2004 observed with GEOTAIL: Do magnetospheric instabilities trigger large scale fracturing of magnetar's crust?
Y. T. Tanaka, T. Terasawa, N. Kawai, A. Yoshida, I. Yoshikawa, Y., Saito, T. Takashima, and T. Mukai

TL;DR
This study analyzes the initial spike profiles of two giant flares from magnetars, revealing distinct phases likely caused by magnetospheric activity and crustal fracturing, and discusses implications for identifying extragalactic SGR flares.
Contribution
It provides a detailed comparison of initial spike structures of two SGR giant flares, linking phases to physical origins and suggesting a method to identify extragalactic flares among short GRBs.
Findings
Initial spike profile shows four characteristic structures.
Timescales indicate magnetospheric and crustal origins.
Provides a potential signature for extragalactic SGR flares.
Abstract
We present the unsaturated peak profile of SGR 1900+14 giant flare on 1998 August 27. This was obtained by particle counters of the Low Energy Particle instrument onboard the GEOTAIL spacecraft. The observed peak profile revealed four characteristic structures: initial steep rise, intermediate rise to the peak, exponential decay and small hump in the decay phase. From this light curve, we found that the isotropic peak luminosity was erg s and the total energy was erg s ( 50 keV), assuming that the distance to SGR 1900+14 is 15 kpc and that the spectrum is optically thin thermal bremsstrahlung with 240 keV. These are consistent with the previously reported lower limits derived from Ulysses and Konus-Wind observations. A comparative study of the initial spikes of SGR 1900+14 giant flare in 1998 and SGR 1806-20 in 2004…
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