Compression fronts from fast radio bursts
Andrei M. Beloborodov
TL;DR
This work analyzes how ultrastrong FRB waves interact with magnetar winds, revealing a two-regime picture: stochastic heating and regular oscillations that drive a propagating compression front in the wind. By coupling microphysical particle heating in the fluid frame to macroscopic MHD evolution in a stationary wave packet, the authors derive a steady-front solution and show its relaxation dynamics, including radiative losses and memory effects. The study identifies critical radii, $r_{\rm damp}\sim10^{11}$ cm, $r_{\rm stoch}\sim10^{12}$ cm, and $r_{\star}\sim10^{13}$ cm, which demarcate damping, stochastic heating, and quasisteady compression zones, and demonstrates that FRBs must originate outside the damping zone to escape through magnetar winds. The results constrain FRB emission radii and link plasma heating, wave damping, and compression to observable FRB energetics, with implications for FRB progenitor models and wind parameters. Overall, the paper provides a self-consistent framework for predicting FRB propagation effects in magnetized, relativistic winds.
Abstract
When a fast radio burst (FRB) expands from its source through a surrounding tenuous plasma, it strongly heats and compresses the plasma at radii up to $\sim 10^{14}$cm. The likely central engines of FRBs are magnetars, and their ambient plasma at radii $r\gg 10^{10}$cm is a magnetized $e^\pm$ wind. We formulate basic equations of the FRB-plasma interaction, solve them numerically, and describe the physical picture of the interaction. We find the following: (1) FRBs emitted at $r<r_{\rm stoch}\sim 10^{12}$cm induce fast stochastic heating and strong compression of the wind, sweeping it like a broom. The outcome of this interaction is determined by the energy losses of the radio wave; we evaluate the parameter space where FRBs survive and escape. (2) At radii $r>r_{\rm stoch}$, FRB induces regular particle oscillations in the radio wave with the standard strength parameter $a$, and drives a compression wave in the wind. At $r>r_\star\sim 10^{13}$cm, the compression wave becomes locally quasisteady, with compression factor $1+a^2$. FRBs avoid damping if they are released into the wind medium outside $r_{\rm damp}\sim 10^{11}$cm.
