Skip to content
DraconiticResearch
Search Sources API
203,234 studies31 sourcesUpdated 2 min ago
PreprintCC BY 4.0arXiv

Magnetically Confined Mountains on Accreting White Dwarfs

Abstract

The hydromagnetic structure of magnetically confined mountains on accreting white dwarfs is computed, alongside the effects of accretion on the reduction of the star's magnetic field. The equilibrium structure of the mountain is obtained by numerically solving the Grad-Shafranov equation with a self-consistent scheme that enforces magnetic flux freezing. For characteristic system parameters, it is shown that magnetic field lines are significantly deformed and dragged equatorwards by mountains with masses ∼10−3M⊙ that have a characteristic height of ∼105 cm. A mathematical relation is obtained for the maximum mass that a white dwarf can confine magnetically given the star's magnetic field and temperature. It is found that the accretion buries the star's magnetic field by reducing it by up to 10% of its pre-accretion value. The star's magnetic field remains dominantly dipolar, but with added multipolar components.

Related

  1. Gravitational Waves from Magnetically Confined Mountains on Accreting White Dwarfs
    Pedro Henrique Barboza Rossetto, Manoel Felipe Sousa, Diego Antonio Falceta Gonçalves
    arXivPreprintCC BY 4.0Full textHigh-energy astrophysicsSolar & stellar physicsarXiv
  2. Discovery of a second-generation planet candidate accreting onto a white dwarf
    Jamie T. Williams, Boris T. Gänsicke, Nicholas C. Stone +10
    arXivPreprintarXiv licenceFull textPlanetary science & exoplanetsSolar & stellar physicsarXiv
  3. Temperature effects on white dwarfs in modified gravity
    Sofía Vidal, Aneta Wojnar, Laur Järv
    arXivPreprintCC BY 4.0Full textSolar & stellar physicsGravitation & general relativityarXiv
  4. Tidal Properties of White Dwarfs Admixed with Fermionic Dark Matter
    G. A. Carvalho, J. D. V. Arbañil, I. A. Lacerda +1
    arXivPreprintCC BY 4.0Full textSolar & stellar physicsarXiv
  5. Slowly rotating white dwarfs in f (R, T ) = R + 2λT gravity: structure and stationary tidal response
    Edson Otoniel, Jonathan A. Rebouças, P. H. R. S. Moraes
    arXivPreprintarXiv licenceFull textHigh-energy astrophysicsSolar & stellar physicsarXiv
BibTeX
@misc{rossetto2026magnetically,
  title = {{Magnetically Confined Mountains on Accreting White Dwarfs}},
  author = {Pedro H. B. Rossetto and Manoel F. Sousa and Diego A. Falceta-Gonçalves},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.05868},
  eprint = {2609.05868},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.05868},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Magnetically Confined Mountains on Accreting White Dwarfs
AU  - Pedro H. B. Rossetto
AU  - Manoel F. Sousa
AU  - Diego A. Falceta-Gonçalves
PY  - 2026
DA  - 2026/09/05
PB  - arXiv
DO  - 10.48550/arxiv.2609.05868
UR  - https://arxiv.org/abs/2609.05868
AB  - The hydromagnetic structure of magnetically confined mountains on accreting white dwarfs is computed, alongside the effects of accretion on the reduction of the star's magnetic field. The equilibrium structure of the mountain is obtained by numerically solving the Grad-Shafranov equation with a self-consistent scheme that enforces magnetic flux freezing. For characteristic system parameters, it is shown that magnetic field lines are significantly deformed and dragged equatorwards by mountains with masses ∼10^−3M_⊙ that have a characteristic height of ∼10^5 cm. A mathematical relation is obtained for the maximum mass that a white dwarf can confine magnetically given the star's magnetic field and temperature. It is found that the accretion buries the star's magnetic field by reducing it by up to 10% of its pre-accretion value. The star's magnetic field remains dominantly dipolar, but with added multipolar components.
ER  -