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Modeling helioseismic modes in the magnetic atmosphere of the Sun
Author(s) -
Pintér B.
Publication year - 2007
Publication title -
astronomische nachrichten
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.394
H-Index - 63
eISSN - 1521-3994
pISSN - 0004-6337
DOI - 10.1002/asna.200710784
Subject(s) - physics , solar atmosphere , atmosphere (unit) , oscillation (cell signaling) , magnetohydrodynamic drive , helioseismology , magnetohydrodynamics , magnetic field , coupling (piping) , computational physics , astrophysics , line (geometry) , mode (computer interface) , meteorology , mechanical engineering , geometry , mathematics , quantum mechanics , biology , engineering , genetics , computer science , operating system
The pulsation of the solar surface is caused by acoustic waves traveling in the solar interior. Thorough analyses of observational data indicate that these f and p helioseismic oscillation modes are not bounced back completely at the surface but they partially penetrate into the atmosphere. Atmospheric effects and their possible observational application are investigated in one‐dimensional magnetohydrodynamic models. It is found that f and p mode frequencies are shifted of the order of μHz due to the presence of an atmospheric magnetic field. This shift varies with the direction of the wave propagation.Resonant coupling of global helioseismic modes to local Alfvén and slow waves reduce the life time of the global modes. The resulting line width of the frequency line is of the order of nHz, and it also varies with propagation angle. These features enable us to use helioseismic observations in magnetic diagnostics of the lower atmosphere. (© 2007 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)