Planetary Geoid

Planetary Geoid is the equipotential surface of a planet's gravity field that best approximates the mean shape of its fluid envelope, distinguishing itself from other reference surfaces by representing the global mean sea level in the absence of tidal, atmospheric, and dynamic oceanic forces.

45

Publications

2.5K

Citations

107

Authors

57

Institutions

Publications per year

2017–2026

2

Authors

107

  1. BH
    Bradford H. Hager

    Massachusetts Institute of Technology, United States

    3 publications · 243 citations

    3

    h-index

  2. PV
    Petr Vaníček

    University of New Brunswick, Canada

    2 publications · 93 citations

    3

    h-index

  3. AA
    Alireza A. Ardalan

    University of Tehran, Iran

    1 publications · 17 citations

    2

    h-index

  4. ZM
    Z. Martinec

    Charles University, Czechia

    2 publications · 93 citations

    2

    h-index

  5. WS
    W. S. Kiefer

    Lunar and Planetary Institute, United States

    2 publications · 164 citations

    2

    h-index

1–5 of 107

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 12 publications · 1.1K citations

    11

    h-index

  2. Geophysical Research Letters

    5 publications · 299 citations

    5

    h-index

  3. Journal of Geodesy

    4 publications · 256 citations

    4

    h-index

  4. Science

    3 publications · 386 citations

    3

    h-index

  5. Surveys in Geophysics

    2 publications · 32 citations

    2

    h-index

1–5