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Direct assessment of SDO/HMI helioseismology of active regions on the Sun's far side using SO/PHI magnetograms

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Direct assessment of SDO/HMI helioseismology of active regions on the Sun's far side using SO/PHI magnetograms

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dc.contributor.author Yang, D.
dc.contributor.author Blanco Rodríguez, Julian
dc.contributor.author Gasent-Blesa, José Luis
dc.contributor.author Sanchis Kilders, Esteban
dc.contributor.author Orozco Suárez, D.
dc.contributor.author Alvarez Herrero, A.
dc.contributor.author Albelo Jorge, N.
dc.contributor.author del Toro Iniesta, J. C.
dc.contributor.author Gutiérrez Márquez, P.
dc.contributor.author Solanki, S.K.
dc.contributor.author Bellot Rubio, L.R.
dc.contributor.author Pérez Grande, Isabel
dc.date.accessioned 2023-11-27T10:57:40Z
dc.date.available 2023-11-27T10:57:40Z
dc.date.issued 2023
dc.identifier.uri https://hdl.handle.net/10550/91450
dc.description.abstract Context. Earth-side observations of solar p modes can be used to image and monitor magnetic activity on the Sun's far side. In this work, we use magnetograms of the far side obtained by the Polarimetric and Helioseismic Imager (PHI) on board Solar Orbiter (SO) to directly assess the validity of far-side helioseismic holography for the first time. Aims. We wish to co-locate the positions of active regions in helioseismic images and magnetograms and to calibrate the helioseismic measurements in terms of the magnetic field strength. Methods. We identified three magnetograms displaying a total of six active regions on the far side from 18 November 2020, 3 October 2021, and 3 February 2022. The first two dates are from the SO cruise phase and the third is from the beginning of the nominal operation phase. We computed contemporaneous seismic phase maps for these three dates using helioseismic holography applied to the time series of Dopplergrams from the Helioseismic and Magnetic Imager (HMI) at the Solar Dynamics Observatory (SDO). Results. Among the six active regions seen in SO/PHI magnetograms, five of them are identified on the seismic maps at almost the same positions as on the magnetograms. One region is too weak to be detected above the seismic noise. To calibrate the seismic maps, we fit a linear relationship between the seismic phase shifts and the unsigned line-of-sight magnetic field averaged over the active region areas extracted from the SO/PHI magnetograms. Conclusions. SO/PHI provides the strongest evidence so far that helioseismic imaging is able to provide reliable information on active regions on the far side, including their positions, areas, and the mean unsigned magnetic field.
dc.language.iso eng
dc.relation.ispartof Astronomy and Astrophysics, 2023, vol. 674, num. A183, p. 1-9
dc.source Yang, D., Blanco Rodríguez, Julian, Gasent-Blesa, José Luis, Sanchis Kilders, Esteban, Orozco Suárez, D., Alvarez Herrero, A., Albelo Jorge, N., del Toro Iniesta, J.C., Gutiérrez Márquez, P., Solanki, S.K., Bellot Rubio, L.R., Pérez Grande, Isabel (2023). Direct assessment of SDO/HMI helioseismology of active regions on the Sun's far side using SO/PHI magnetograms. Astronomy and Astrophysics, 674 A183 1 9. https://doi.org/10.1051/0004-6361/202346030
dc.subject astronomia
dc.subject física
dc.subject Física
dc.subject electrònica
dc.subject helioseismology
dc.subject photosphere
dc.subject magnetic fields
dc.subject sun activity
dc.title Direct assessment of SDO/HMI helioseismology of active regions on the Sun's far side using SO/PHI magnetograms
dc.type journal article
dc.date.updated 2023-11-27T10:57:40Z
dc.identifier.doi 10.1051/0004-6361/202346030
dc.identifier.idgrec 162133
dc.rights.accessRights open access

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