Prominence Oscillations: Effect of a Time-dependent Background Temperature

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dc.contributor.author Ballester, J. L.
dc.contributor.author Carbonell, M.
dc.contributor.author Soler, R.
dc.contributor.author Terradas, J.
dc.date.accessioned 2025-01-30T14:14:48Z
dc.date.available 2025-01-30T14:14:48Z
dc.identifier.citation Ballester, J. L., Carbonell, M., Soler, R., i Terradas, J. (2016). Prominence oscillations: Effect of a time-dependent background temperature. Astronomy & Astrophysics, 591(A109), 1-12. https://doi.org/10.1051/0004-6361/201527953 ca
dc.identifier.uri http://hdl.handle.net/11201/168327
dc.description.abstract [eng] Context. Small amplitude oscillations in prominences have been known about for a long time, and from a theoretical point of view, these oscillations have been interpreted in terms of standing or propagating linear magnetohydrodynamic (MHD) waves. In general, these oscillations were studied by producing small perturbations in a background equilibrium with stationary physical properties. Aims: Taking into account that prominences are dynamic plasma structures, the assumption of a stationary equilibrium is not realistic. Therefore, our main aim is to study the effects produced by a non-stationary background on slow MHD waves, which could be responsible for prominence oscillations. Methods: Assuming that the radiation term is proportional to temperature and constant external heating, we have derived an expression for the temporal variation of the background temperature, which depends on the imbalance between heating and cooling processes. Furthermore, radiative losses, together with parallel thermal conduction, have also been included as damping mechanisms for the waves. Results: As temperature increases with time, the period of slow waves decreases and the amplitude of the velocity perturbations is damped. The inclusion of radiative losses enhances the damping. As temperature decreases with time, the period of slow waves increases and the amplitude of velocity perturbations grows while, as expected, the inclusion of radiative losses contributes to the damping of oscillations. Conclusions: There is observational evidence that, in different locations of the same prominence, oscillations are damped or amplified with time. This temporal damping or amplification can be obtained by a proper combination of a variable background temperature, together with radiative damping. Furthermore, decayless oscillations can also be obtained with an appropriate choice of the characteristic radiation time. en
dc.format application/pdf
dc.publisher European Southern Observatory
dc.relation.ispartof Astronomy & Astrophysics, 2016, vol. 591, num. A109, p. 1-12
dc.rights all rights reserved
dc.subject.classification 53 - Física
dc.subject.classification 52 - Astronomia. Astrofísica. Investigació espacial. Geodèsia
dc.subject.other 53 - Physics
dc.subject.other 52 - Astronomy. Astrophysics. Space research. Geodesy
dc.title Prominence Oscillations: Effect of a Time-dependent Background Temperature en
dc.type info:eu-repo/semantics/article
dc.type info:eu-repo/semantics/acceptedVersion
dc.type Article
dc.date.updated 2025-01-30T14:14:49Z
dc.rights.accessRights info:eu-repo/semantics/openAccess
dc.identifier.doi https://doi.org/10.1051/0004-6361/201527953


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