Pole Tide
Pole Tide is a geodetic phenomenon representing the deformation of the Earth's surface and gravitational field due to polar motion, distinguished from other tidal components by its direct association with shifts in the planet's rotational axis rather than lunisolar gravitational forcing.
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3.6K
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113
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66
Institutions
Publications per year
2017–2026
3
Variants
Pole Tides
Parents
58
The period and Q of the Chandler wobble
Melvyn Smith, F. A. Dahlen · Geophysical Journal International · 1981 · 308 citations
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University of Colorado Boulder
Boulder, United States
5 h-index
8 publications
656 citations
The University of Texas at Austin
Austin, United States
5 h-index
11 publications
2K citations
Binghamton University
Binghamton, United States
5 h-index
7 publications
222 citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
5 h-index
6 publications
748 citations
Jet Propulsion Laboratory
Pasadena, United States
4 h-index
4 publications
1.1K citations
Institute of Geodesy and Geophysics
Wuhan, China
4 h-index
10 publications
192 citations
Goddard Space Flight Center
Greenbelt, United States
4 h-index
5 publications
114 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
7 publications
130 citations
1–8 of 66
GJI · 22 publications · 1.4K citations
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JGR · 10 publications · 1.5K citations
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4 publications · 159 citations
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4 publications · 143 citations
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3 publications · 43 citations
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