極正距方位図法によって表わした北半球北部のアルチメトリィジオイド〔英文〕
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概要
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Geoid for the areas of the northern part of North Hemisphere has been evaluated and mapped by means of polar azimuthal equidistant projection using SEASAT altimeter data covering north of 45°N. The relative accuracy of the geoid obtained expressed by 1σ value of the crossover errors varies from 35 to 131 cm, depending on local topographic situations. The geoid presented here has been compared with the geoid published in 1982 by R. H. Rapp of the Ohio State University. This geoid map is useful parti cularly when geodetic and geophysical features of the northernmost regions such as the Okhotsk Sea, the Bering Sea, the northern Atlantic or the Arctic Sea are discussed.
- 日本測地学会の論文
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