Time-distance helioseismology and the magnetic atmoŝphere of the sun
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Time-distance helioseismology and the magnetic atmoŝphere of the sun. / Taroyan, Y.; Erdélyi, R.; Doyle, J. G.
Proceedings of the Conference SOHO 13 - Waves, Oscillations and Small-Scale Transient Events in the Solar Atmosphere: A Joint View from SOHO and TRACE. 547. ed. 2004. p. 33-38 (European Space Agency, (Special Publication) ESA SP).Research output: Chapter in Book/Report/Conference proceeding › Conference Proceeding (Non-Journal item)
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TY - GEN
T1 - Time-distance helioseismology and the magnetic atmoŝphere of the sun
AU - Taroyan, Y.
AU - Erdélyi, R.
AU - Doyle, J. G.
N1 - Copyright: Copyright 2008 Elsevier B.V., All rights reserved.
PY - 2004
Y1 - 2004
N2 - In time-distance helioseismology the travel time of the acoustic waves between different points on the solar surface is measured to infer the local structure and properties of the subsurface layers of the Sun. The presence of the magnetic canopy in the solar atmosphere is expected to modify the behavior of the acoustic waves. The travel time changes due to the atmospheric magnetic field are evaluated theoretically. The uniform magnetic field in the atmosphere shortens the travel time of the acoustic waves due to enhanced rigidity of the interface where the waves are reflected. This effect increases rapidly with increasing frequency and harmonic degree. The effect of the magnetic field on the acoustic wave travel time is compared with the corresponding effect of large-scale sub-surface flows. It is suggested to use the time-distance analysis as a diagnostic tool in determining the local properties of the Sun's atmospheric magnetic field.
AB - In time-distance helioseismology the travel time of the acoustic waves between different points on the solar surface is measured to infer the local structure and properties of the subsurface layers of the Sun. The presence of the magnetic canopy in the solar atmosphere is expected to modify the behavior of the acoustic waves. The travel time changes due to the atmospheric magnetic field are evaluated theoretically. The uniform magnetic field in the atmosphere shortens the travel time of the acoustic waves due to enhanced rigidity of the interface where the waves are reflected. This effect increases rapidly with increasing frequency and harmonic degree. The effect of the magnetic field on the acoustic wave travel time is compared with the corresponding effect of large-scale sub-surface flows. It is suggested to use the time-distance analysis as a diagnostic tool in determining the local properties of the Sun's atmospheric magnetic field.
KW - Magnetic canopy
KW - Sun
KW - Time-distance helioseismology
UR - http://www.scopus.com/inward/record.url?scp=18644362406&partnerID=8YFLogxK
M3 - Conference Proceeding (Non-Journal item)
AN - SCOPUS:18644362406
T3 - European Space Agency, (Special Publication) ESA SP
SP - 33
EP - 38
BT - Proceedings of the Conference SOHO 13 - Waves, Oscillations and Small-Scale Transient Events in the Solar Atmosphere:
T2 - Proceedings of the Conference SOHO 13 - Waves, Oscillations and Small-Scale Transient Events in the Solar Atmosphere: A Joint View from SOHO and TRACE
Y2 - 29 September 2003 through 3 October 2003
ER -