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A Comparison of Solar<i>p</i>‐Mode Parameters from MDI and GONG: Mode Frequencies and Structure Inversions

Sarbani BasuDepartment of Astronomy, Yale University, P.O. Box 208101, New Haven, CT 06520-8101J. Christensen‐DalsgaardInstitut for Fysik og Astronomi, Aarhus Universitet, DK-8000 Aarhus C, Denmark, and Teoretisk Astrofysik Center, Danmarks GrundforskningsfondR. HoweNational Solar Observatory, 950 North Cherry Avenue, Tucson, AZ 85719J. SchouHEPL Annex A201, Stanford University, Stanford, CA 94305-4085M. J. ThompsonSpace and Atmospheric Physics Group, Blackett Laboratory, Imperial College, London SW7 2BW, UKF. HillNational Solar Observatory, 950 North Cherry Avenue, Tucson, AZ 85719R. KommNational Solar Observatory, 950 North Cherry Avenue, Tucson, AZ 85719
2003en
ABI

Аннотация

Helioseismic analysis of solar global oscillations allows investigation of the internal structure of the Sun. One important test of the reliability of the inferences from helioseismology is that the results from independent sets of contemporaneous data are consistent with one another. Here we compare mode frequencies from the Global Oscillation Network Group and Michelson Doppler Imager on board SOHO and resulting inversion results on the Sun's internal structure. The average relative differences between the data sets are typically less than 1 × 10-5, substantially smaller than the formal errors in the differences; however, in some cases the frequency differences show a systematic behavior that might nonetheless influence the inversion results. We find that the differences in frequencies are not a result of instrumental effects but are almost entirely related to the data pipeline software. Inversion of the frequencies shows that their differences do not result in any significant effects on the resulting inferences on solar structure. We have also experimented with fitting asymmetric profiles to the oscillation power spectra and find that, compared with the symmetric fits, this causes no significant change in the inversion results.

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