geoid वाक्य
उदाहरण वाक्य
मोबाइल
- If the mantle were static, these low-density regions would be geoid lows.
- The Earth geoid is essentially the figure of the Earth abstracted from its topographic features.
- Experimental determination of the gravitational potential at the geoid surface is a task in physical geodesy.
- This allows direct measurement of the geoid, since the ocean surface closely follows the geoid.
- This allows direct measurement of the geoid, since the ocean surface closely follows the geoid.
- The earth does not have a perfect ellipsoidal shape, but is described as a geoid.
- A rise in sea level, however, would expand the geoid and mean sea level.
- :See geoid and equipotential surface.
- Therefore, the Mars geoid is essentially the figure of Mars abstracted from its topographic features.
- :: WGS 84 measures the reference ellipsoid of the geoid, not the Earth itself.
- The reference surface for orthometric heights is the geoid, an equipotential surface approximating mean sea level.
- The deviations of the geoid from the first order spheroid are on the order of ?100m.
- Dynamic topography is the reason why the geoid is high over regions of low-density mantle.
- Ocean surface topography is specifically the distance between the height of the ocean surface from the geoid.
- Sea level can also be measured by satellites using radar altimetry, contributing to a more accurate geoid.
- Currently, WGS 84 uses the EGM96 ( Earth Gravitational Model 1996 ) geoid, revised in 2004.
- It is then possible to compute the geoid height by subtracting the measured altitude from the ellipsoidal height.
- Spatial variations in gravity exert influence on the ocean surface and thereby cause spatial structure in the geoid.
- They are used in gravity surveys over large areas for establishing the figure of the geoid over these areas.
- This terminology is also used for such approximately spheroidal astronomical bodies as the planet Earth ( see geoid ).
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