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Publikováno v:
Journal of Information System and Technology Management. 6:226-242
The description of the earth’s gravity field is usually expressed in terms of spherical harmonic coefficients, derived from global geopotential models. These coefficients may be used to evaluate such quantities as geoid undulations, gravity anomali
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5a2ccfaf260bd1658c1427d09de217f9
https://doi.org/10.35631/jistm.624022
https://doi.org/10.35631/jistm.624022
