z-logo
Premium
Variations of the solid Earth's center of mass due to oceanic tides
Author(s) -
Brosche P.,
Wünsch J.
Publication year - 1993
Publication title -
astronomische nachrichten
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.394
H-Index - 63
eISSN - 1521-3994
pISSN - 0004-6337
DOI - 10.1002/asna.2113140206
Subject(s) - center (category theory) , solid earth , geology , earth (classical element) , astrobiology , physics , geodesy , astronomy , environmental science , geophysics , chemistry , crystallography
Periodic variations in the location of the center of mass of the solid Earth due to ocean tides are derived from the ocean tide model of Seiler (1991). The sum of nine partial tides leads to changes in the coordinates X, Y, Z within a range of 1cm.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here