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Constant part of the Earth tides in the Earth figure theory
Summary It is recommended not to reduce measured geodetic values by the constant part of the tidal influence. For this case there is shown an exact solution of the tasks of the theory of the Earth figure, which leads to introducing simple corrections of the gravity anomalies but only for the solution of the boundary value problem.
Constant part of the Earth tides in the Earth figure theory
Summary It is recommended not to reduce measured geodetic values by the constant part of the tidal influence. For this case there is shown an exact solution of the tasks of the theory of the Earth figure, which leads to introducing simple corrections of the gravity anomalies but only for the solution of the boundary value problem.
Constant part of the Earth tides in the Earth figure theory
Yurkina, M. I. (author) / Šimon, Z. (author) / Zeman, A. (author)
Bulletin Gæodésique ; 60
1986
Article (Journal)
English
Geodäsie , Geometrie , Geodynamik , Zeitschrift , Mathematik , Mineralogie
Constant part of the Earth tides in the Earth figure theory
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