Fast Radio Bursts from non-resonant Alfvén waves and synchrotron maser emission in the magnetar wind
Killian Long, Asaf Pe'er
TL;DR
This paper proposes that fast radio bursts (FRBs) originate from synchrotron maser emission (SME) generated by non-resonant interactions between Alfvén waves and the relativistic magnetar wind, producing a crescent-shaped population inversion that drives SME. By calculating growth rates across a parameter space defined by temperature $\theta$, magnetisation $\sigma$, and wind Lorentz factor $\gamma_w$, the authors derive conditions under which SME can operate and emit at GHz frequencies, finding a minimum $\gamma_w \gtrsim 3\times 10^2$ and a low $\theta$ window ($\theta \lesssim 0.02$). They then impose FRB constraints on frequency, timescale, and emission-site size to bound the emission radius $R_{FRB}$ and assess whether the magnetosphere must be perturbed by flaring activity; applying the framework to FRB 20200428 shows that a perturbed magnetosphere greatly eases the required wind properties. The results connect FRB observables to the wind conditions near magnetars and offer a diagnostic for magnetar environments, while highlighting the roles of O-mode and X-mode SME and the need for relativistic winds beyond the light cylinder.
Abstract
Non-resonant interactions between Alfvén waves and a relativistic plasma result in the formation of the population inversions necessary for synchrotron maser emission (SME) across a wide range of magnetisations and temperatures. We calculate the peak frequencies of the SME resulting from this interaction and show that the characteristic frequencies and energetics of fast radio bursts (FRBs) can be produced in the relativistic wind of a magnetar using this mechanism. Wind Lorentz factors of $γ_w\gtrsim310$ are shown to be necessary to explain observed FRBs. Emission is possible at temperatures of $θ= k_bT/mc^2\lesssim 0.02$. We further examine the periods and magnetic fields of the central magnetar and demonstrate that the optimal values of these properties align with the observed magnetar population provided that the magnetosphere is disturbed by the flaring activity. These results allow the properties of the environment such as temperature and magnetisation to be probed from the observed FRB frequency and luminosity.
