In this study, the accuracy of the three known approximate formulae for calculating dynamic heights in the normal gravity field of the Earth for a level ellipsoid of the system WGS-84 is investigated. A simple formula is proposed for the calculation of dynamic heights, the standard deviation of which for geodetic heights varying from 0 to 100 km does not exceed 0.1 m. This formula can be successfully applied not only in geodesy but also in meteorology.
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