Abstract
AbstractBasically, there are two approaches for the analysis of helioseismic data. First, local helioseismology measurements and inversions and, second, global helioseismology which consists in measurements and inversions of p‐mode frequencies and frequency splittings. Both the advantages and disadvantages of global helioseismology and the local technique of ringdiagram analysis are discussed. Also discussed are two fitting methodologies for use in global helioseismology. Finally, a modification of the traditional global helioseismology approach is suggested which allows the extension of spherical harmonic decompositions for local helioseismic studies. (© 2007 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
