A gravimetric terrain correction method by assuming annular prism model.
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概要
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A computation program of terrain correction by assuming the annular prism model was made to be applied to the gravity station not only on the ground but also in the tunnel, on the bottom of the sea, on the surface of the sea or in the air. The calculation region of terrain correction is composed of following four regions. The extreme-near region including gravity station is from 0 m to 500 m, the near region is from 500 m to 4 km, the intermediate region is from 4 km to 16 km, and the far region is from 16 km to 60 km. At first, three kinds of terrain data, which are read from grids of latitude and longitude (7.5X11.25" (near), 30"X45" (intermediate), 2'X3' (far)), are transf omed into UTM coordinate and stored in an external memory device (disk). At next stage, three kinds of new terrain mesh data (mesh size; 125 m (near), 500 m (intermediate), 2km (far)) are formed from three kinds of original terrain data stored in the external memory device by the interpolation of weighted averaging method, and those formed mesh data are stored in internal memory device. Annular prism models around the station are assumed from newly-formed terrain mesh data stored in the internal memory by weighted averaging method, and annular prisms within 125 m from the station are assumed not only newly-formed mesh but also the station terrain data (the surface height of the ground or the water). At last, gravity values are calculated from annular prism models and summed up. Error of values of this terrain correction is expected to be within 2 mgals when KS-110 terrain data are used as the original terrain data for the terrain correction.
- 日本測地学会の論文
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