期刊
SOLAR PHYSICS
卷 296, 期 11, 页码 -出版社
SPRINGER
DOI: 10.1007/s11207-021-01901-6
关键词
Magnetic fields, photosphere; Instrumentation and data management; Instrumental effects
资金
- RFBR of Russia
- NNSF of China
- Russian Fund for Basic Research [17-52-53203, 19-52-53045]
- National Natural Science Foundation of China [11673033, U1731113, 11611530679, 11573037, 11703042, 119115300890, 12073041, 11427901, 10921303, 12073040]
- Strategic Priority Research Program of Chinese Academy of Sciences [XDB09040200, XDA04061002, XDA15010700]
- Youth Innovation Promotion Association of CAS [2019059]
- Russian Science Foundation [18-12-00131]
This study aims to improve magnetic field observations made by the Solar Magnetic Field Telescope (SMFT) at the Huairou Solar Observing Station in China, proposing the use of a non-linear relationship for deriving the magnetic field and cross-calibrating observations with magnetograms from the Solar Dynamics Observatory. The non-linear relationship effectively eliminates magnetic field saturation within sunspot umbrae.
The weak-field approximation, implying a linear relationship between Stokes- V/I and the longitudinal magnetic field [B-parallel to], often suffers from saturation observed in strong magneticfield regions such as sunspot umbrae. In this work, we seek to improve the magnetic-field observations carried out by the Solar Magnetic Field Telescope (SMFT) at the Huairou Solar Observing Station, China. We propose using a non-linear relationship between Stokes-V/I and B-parallel to to derive the magnetic field. To determine the form of the relationship, we perform a cross-calibration of the observed SMFT data and magnetograms provided by the Helioseismic and Magnetic Imager onboard the Solar Dynamics Observatory. The algorithm for the magnetic-field derivation is described in detail. We show that using a non-linear relationship between Stokes-V/I and B-parallel to allows us to eliminate magnetic-field saturation inside the sunspot umbra. The proposed technique enables one to enhance the reliability of the SMFT magnetic-field data obtained even long before the space-based instrumentation era, since 1987.
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