geoid wikipedia - EAS

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    https://en.wikipedia.org/wiki/Geoid

    The geoid is the shape that the ocean surface would take under the influence of the gravity of Earth, including gravitational attraction and Earth's rotation, if other influences such as winds and tides were absent. This surface is extended through the continents (such as with very narrow

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    The geoid surface is irregular, unlike the reference ellipsoid (which is a mathematical idealized representation of the physical Earth as an ellipsoid), but is considerably smoother than Earth's physical surface. Although

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    Calculating the undulation is mathematically challenging. This is why many handheld GPS receivers have built-in undulation lookup tables to determine the height above sea level.

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    Recent satellite missions, such as the Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) and GRACE, have enabled the study of time-variable geoid signals. The first

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    Spherical harmonics are often used to approximate the shape of the geoid. The current best such set of spherical harmonic coefficients is EGM2020 (Earth Gravity Model 2020),

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  2. https://simple.wikipedia.org/wiki/Geoid

    Geoid From Simple English Wikipedia, the free encyclopedia Flattened sphere (exaggerated) The geoid is a shape like the surface of the Earth. It is a 3-D geometrical shape like an orange. Shapes of this kind are called oblate spheroids, which is a kind of ellipsoid. The geoid, however, is a very special kind of oblate spheroid.

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      What is a geoid?
      The geoid ( / ˈdʒiːɔɪd /) is the shape that the ocean surface would take under the influence of the gravity of Earth, including gravitational attraction and Earth's rotation, if other influences such as winds and tides were absent. This surface is extended through the continents (such as with very narrow hypothetical canals).
      en.wikipedia.org/wiki/Geoid
      Search for: What is a geoid?
      What is the geoid's radius?
      being the geocentric radius, i.e., distance from the Earth's centre. The geoid is a particular equipotential surface, and is somewhat involved to compute. The gradient of this potential also provides a model of the gravitational acceleration.
      en.wikipedia.org/wiki/Geoid
      What is a geode formation?
      Geodes (derived from the Greek word "γεώδης" meaning "Earth-like") are geological secondary formations within sedimentary and volcanic rocks. Geodes are hollow, vaguely spherical rocks, in which masses of mineral matter (which may include crystals) are secluded.
      en.wikipedia.org/wiki/Geode
      What is the shape of the geoid undulation?
      Geoid undulation (red) relative to the reference ellipsoid (black). Spherical harmonics are often used to approximate the shape of the geoid.
      en.wikipedia.org/wiki/Geoid
    • https://sv.wikipedia.org/wiki/Geoid

      En geoid (av grekiska: geo, jord och eides, liknande) är en yta som ungefär sammanfaller med havsytans genomsnittliga nivå. Den sägs ofta vara en nära återgivning eller fysisk modell av jordens äkta form och enligt Carl Friedrich Gauss är geoiden en "matematisk bild av jorden" eller, egentligen, av dess gravitationsfält. Geodeter kan beräkna höjden hos punkter på kontinenternaova…

    • https://ro.wikipedia.org/wiki/Geoid
      Image
      Fiecare punct este accelerat pe Pământ la gravitatea g → {\displaystyle {\overrightarrow {g}}} . Această accelerare derivă din potențialul gravitațional W {\displaystyle W} , astfel încât: Suprafețele unde potențialul de gravitate E p = − W {\displaystyle E_{p}=-W} este constant sunt echipotențiale de gravitate. Un geoid e…
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    • https://cs.wikipedia.org/wiki/Geoid

      Geoid je fyzikální model povrchu Země při střední hladině světových oceánů.Je definován jako ekvipotenciální plocha vůči gravitaci, to jest plocha se stejnou úrovní tíhového potenciálu, na kterou je vektor tíhového zrychlení kolmý. Hodnota W 0 geopotenciálu, kterou přijala IAU, je 62636856 m 2 s −2.. Geoid je vlastně reprezentovaný ekvipotenciální plochou ...

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      • https://it.wikipedia.org/wiki/Geoide

        Geoide Da Wikipedia, l'enciclopedia libera. Mappa dell'ondulazione del geoide, in metri (basata sul modello di gravità EGM96 e sull'ellissoide di riferimento WGS84)

      • https://sk.wikipedia.org/wiki/Geoid

        Geoid je fyzikálny model povrchu Zeme pri strednej hladine svetových oceánov.Je definovaný ako ekvipotenciálna plocha voči gravitácii, t. j. plocha s rovnakou úrovňou gravitačného potenciálu, na ktorý je vektor tiažového zrýchlenia kolmý.. Geoid, ako matematické teleso aproximujúce zemský povrch, pochádza z roku 1871 z dielne francúzskeho vedca Listinga.



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