Oscillatory Line-Driven Winds: The Role of Atmospheric Stratification

Fuente: arXiv
Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Key, Joshua, Proga, Daniel, Dannen, Randall, Vivier, Sterling, Waters, Timothy
Format: Preprint
Veröffentlicht: 2025
Schlagworte:
Online-Zugang:
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
_version_ 1866915252896006144
author Key, Joshua
Proga, Daniel
Dannen, Randall
Vivier, Sterling
Waters, Timothy
author_facet Key, Joshua
Proga, Daniel
Dannen, Randall
Vivier, Sterling
Waters, Timothy
contents Time-dependent numerical studies of line-driven winds using the Sobolev approximation have a history spanning over three decades. In many of these studies, the wind solutions display notorious oscillations. Two clues suggest the oscillations originate at the wind base: (i) simulations reach a steady state without oscillations when the base density is sufficiently low and (ii) the oscillation dominant frequency is comparable to the Lamb cut-off frequency, ωc, of acoustic waves propagating in a stratified hydrostatic atmosphere. Recently, Dannen et al. observed another clue: when the line force significantly weakens due to ionization, the winds become increasingly sensitive to the self-excited oscillations. Here, we present a set of simulations and perturbation analyses that further elucidate the source and characteristics of oscillations. We found that the line force adds wave energy and amplifies perturbations with frequencies near ωc. This selective amplification results from the coupling between the natural tendency of velocity perturbations to grow in a stratified atmosphere and from the line force dependence on the velocity gradient, per the Castor-Abbott-Klein line-driven wind theory. We also found that the variability stems from self-excitation that occurs in the exponential atmosphere due to the non-linearity introduced by the absolute value of the velocity gradient in the line force prescription. We conclude that self-consistently calculating ionization is insufficient for modeling the dynamics in the subsonic atmosphere. Instead, future wind or unified models should relax the Sobolev approximation, or model the radiative transfer to properly capture the resulting radiation-induced instabilities and dynamics at the wind base.
format Preprint
id arxiv_https___arxiv_org_abs_2501_14901
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Oscillatory Line-Driven Winds: The Role of Atmospheric Stratification
Key, Joshua
Proga, Daniel
Dannen, Randall
Vivier, Sterling
Waters, Timothy
Astrophysics of Galaxies
Time-dependent numerical studies of line-driven winds using the Sobolev approximation have a history spanning over three decades. In many of these studies, the wind solutions display notorious oscillations. Two clues suggest the oscillations originate at the wind base: (i) simulations reach a steady state without oscillations when the base density is sufficiently low and (ii) the oscillation dominant frequency is comparable to the Lamb cut-off frequency, ωc, of acoustic waves propagating in a stratified hydrostatic atmosphere. Recently, Dannen et al. observed another clue: when the line force significantly weakens due to ionization, the winds become increasingly sensitive to the self-excited oscillations. Here, we present a set of simulations and perturbation analyses that further elucidate the source and characteristics of oscillations. We found that the line force adds wave energy and amplifies perturbations with frequencies near ωc. This selective amplification results from the coupling between the natural tendency of velocity perturbations to grow in a stratified atmosphere and from the line force dependence on the velocity gradient, per the Castor-Abbott-Klein line-driven wind theory. We also found that the variability stems from self-excitation that occurs in the exponential atmosphere due to the non-linearity introduced by the absolute value of the velocity gradient in the line force prescription. We conclude that self-consistently calculating ionization is insufficient for modeling the dynamics in the subsonic atmosphere. Instead, future wind or unified models should relax the Sobolev approximation, or model the radiative transfer to properly capture the resulting radiation-induced instabilities and dynamics at the wind base.
title Oscillatory Line-Driven Winds: The Role of Atmospheric Stratification
topic Astrophysics of Galaxies
url https://arxiv.org/abs/2501.14901