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Indian geoid on GRS 67 from geopotential coefficients
Abstract The geoid on GRS 67 for the Indian subcontinent has been determined using the geopotential coefficients of degree and order 52 and 180. A broad comparison has also been made between these geoids and the previously determined generalized gravimetric and detailed astrogeodetic-gravimetric geoids. It has been found that still higher degree and order geopotential coefficient solutions from adequate reliable terrestrial data are required to achieve precision of geodetic standards.
Indian geoid on GRS 67 from geopotential coefficients
Abstract The geoid on GRS 67 for the Indian subcontinent has been determined using the geopotential coefficients of degree and order 52 and 180. A broad comparison has also been made between these geoids and the previously determined generalized gravimetric and detailed astrogeodetic-gravimetric geoids. It has been found that still higher degree and order geopotential coefficient solutions from adequate reliable terrestrial data are required to achieve precision of geodetic standards.
Indian geoid on GRS 67 from geopotential coefficients
Srivastava, A. M. C. (author)
Bulletin géodésique ; 59
1985
Article (Journal)
English
Geodäsie , Geometrie , Geodynamik , Zeitschrift , Mathematik , Mineralogie
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