Magnetar Oscillations I: strongly coupled dynamics of the crust and the core

TL;DR

This paper investigates the complex oscillatory behavior of magnetars during giant flares, focusing on the interaction between crust shear modes and core Alfven modes, revealing new insights into their coupled dynamics and observational signatures.

Contribution

It introduces new findings on edge and gap modes, effects of magnetic field tangling, and the decoupling of core components, advancing understanding of magnetar oscillations and QPOs.

Findings

Global edge modes reside near core Alfven continuum edges.

Multiple gaps in the Alfven continuum can produce discrete gap modes.

Core field tangling enhances discrete mode roles and affects oscillation dynamics.

Abstract

Quasi-Periodic Oscillations (QPOs) observed during Soft Gamma Repeaters giant flares are commonly interpreted as the torsional oscillations of magnetars. The oscillatory motion is influenced by the strong interaction between the shear modes of the crust and Alfven-like modes in the core. We study the dynamics which arises through this interaction, and present several new results: (1) We show that global {\it edge modes} frequently reside near the edges of the core Alfven continuum. (2) We compute the magnetar's oscillatory motion for realistic axisymmetric magnetic field configurations and core density profiles, but with a simplified model of the elastic crust. We show that one may generically get multiple gaps in the Alfven continuum. One obtains discrete global {\it gap modes} if the crustal frequencies belong to the gaps. (3) We show that field tangling in the core enhances the role of the core discrete Alfven modes and reduces the role of the core Alfven continuum in the overall oscillatory dynamics of the magnetar. (4) We demonstrate that the system displays transient and/or drifting QPOs when parts of the spectrum of the core Alfven modes contain discrete modes which are densely and regularly spaced in frequency. (5) We show that if the neutrons are coupled into the core Alfven motion, then the post-flare crustal motion is strongly damped and has a very weak amplitude. Thus magnetar QPOs give evidence that the proton and neutron components in the core are dynamically decoupled and that at least one of them is a quantum fluid. (6) We show that it is difficult to identify the high-frequency 625 Hz QPO as being due to the physical oscillatory mode of the magnetar, if the latter's fluid core consists of the standard proton-neutron-electron mixture and is magnetised to the same extent as the crust. (Abstract abridged)