Damping of strong GHz waves near magnetars and the origin of fast radio bursts
Andrei M. Beloborodov

TL;DR
This paper studies how GHz radio waves from fast radio bursts (FRBs) damp near magnetars, revealing that strong waves are absorbed or dissipated in the magnetosphere unless emitted by relativistic outflows, constraining FRB origins.
Contribution
It provides a detailed analysis of GHz wave damping mechanisms near magnetars, distinguishing between MHD and kinetic regimes, and proposes that observed FRBs originate from relativistic outflows to avoid damping.
Findings
GHz waves are damped in the magnetosphere unless emitted along the magnetic axis.
Strong waves develop plasma shocks and dissipate at specific radii depending on luminosity.
Relativistic outflows allow FRBs to escape damping, explaining observed signals.
Abstract
We investigate how a fast radio burst (FRB) emitted near a magnetar would propagate through its surrounding dipole magnetosphere at radii - cm. First, we show that a GHz burst emitted in the O-mode with luminosity erg/s is immediately damped for all propagation directions except a narrow cone along the magnetic axis. Then we examine bursts in the X-mode. GHz waves propagating near the magnetic equator behave as magnetohydrodynamic (MHD) waves if they have erg/s. The waves develop plasma shocks in each oscillation and dissipate at cm. Waves with lower or propagation directions closer to the magnetic axis do not obey MHD. Instead, they interact with individual particles and require a kinetic description. The kinetic interaction quickly accelerates particles to Lorentz factors - at the expense…
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Taxonomy
TopicsPulsars and Gravitational Waves Research · Earthquake Detection and Analysis · Geomagnetism and Paleomagnetism Studies
