geodetic measurement

It was also to be used to obtain geodetic measurements through orbit analysis.

One other surface is involved in geodetic measurement: the geoid.

Newton's result was confirmed by geodetic measurements in the eighteenth century.

The results of geodetic measurements are given mathematical interpretations.

Earth and space-based geodetic measurements indicate ongoing surface uplift above the at approximately 2 mm/year.

It was launched to a polar orbit, from where it did geomagnetic and geodetic measurements.

Geodetic measurement methods at the V2 projekt in Peenemünde ( 1942)

The latter is particularly important because optical instruments containing gravity-reference leveling devices are commonly used to make geodetic measurements.

On February 22, 2007 the construction of the Augustów bypass expressway began with the taking of geodetic measurements.

It combines the precise determination of the true zenith (geographic or astronomical positioning) with geodetic measurements and coordinate calculations.

In his spare time he made geodetic measurements, astronomical observations, experiments on the propagation speed of sound at different heights and measurements using the barometer.

When geodetic measurements have to be computed on a mathematical reference surface, this surface should have a similar curvature as the regional geoid.

Geodetic measurements show periodic reversals in the motion (i.e., westward movement) of the overthrusting North American Plate.

After Earth and space-based geodetic measurements indicated ongoing surface uplift above the "Socorro Magma Body".

The Macrometer Interferometric Surveyor is a commercial GPS-based system for performing geodetic measurements.

At many of the sites where geodetic measurements are made, Meteorological Data are also collected to aid in the processing of the geodetic data.

It is about ten percent of the Rio Grande extension; there is some evidence of the continuous rifting including young fault scarps, seismicity, high heat flow, and ongoing uplift as established by geodetic measurements.

In 1889 he won the Lalande Prize for astronomy from the French Academy of Sciences; 1901 became director of the Quito (Ecuador) Observatory for the purpose of making geodetic measurements.

As part of this project, geodetic measurements of the citadel were taken and these were combined with satellite imagery, regular photographic imagery and aerial photographs to create a map and digital 3D model of the citadel mound and the houses on top of it.