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All fields Title Creator / Publisher Keyword Year AND OR AND NOT All fields Title Creator / Publisher Keyword Year AND OR AND NOT All fields Title Creator / Publisher Keyword Year AND OR AND NOT All fields Title Creator / Publisher Keyword Year AND OR AND NOT All fields Title Creator / Publisher Keyword Year Sort by creator [A → Z]' creator [Z → A]' publishing year ↑ (asc)' publishing year ↓ (desc)' title [A → Z]' title [Z → A]' Simple Search Hits 1 – 3 of 3 1 ON THE NUMERICAL SOLUTION OF MOLODENSKII'S INTEGRAL EQUATION FOR LAYER DENSITY (K Voprosu o Chislennom Reshenii Integralnogo Uraveniya Molodenskogo dlya Plotnosti Sloya) Eremeev,V. F. In: DTIC AND NTIS (1969) BASE Show details 2 REFINEMENT OF MOLODENSKII'S INTEGRAL FORMULAS FOR RADIAL AND LENGTHWISE DISPLACEMENTS (Utochenie Integralnykh Formul Molodenskogo dlya Radialnogo i Prodolnogo Sdvigov) Eremeev,V. F.; Yurkina,M. I. In: DTIC AND NTIS (1969) BASE Show details 3 ON THE DERIVATION OF THE BOUNDARY CONDITION IN THE EARTH FIGURE THEORY (O Vyvode Granichnogo Usloviya Teorii Figury Zemli) Eremeev,V. F.; Yurkina,M. I. In: DTIC AND NTIS (1969) Abstract: The boundary condition for the disturbing potential used in the theory of the earth's figure may be set up for the surface to be determined, and need not be referred to the sphere or ellipsoid in the case of determining a regularized geoid, nor to the surface which is obtained by plotting only normal heights from the reference surface when studying the earth's surface and its exterior gravity field. Errors arising from integration on an unknown surface do not exceed the products T zeta/R or TO, where zeta is the quasigeoidal or geoidal height, R is the earth's radius, and O is the plumbline deflection. The above errors are evaluated in more detail in the case of Molodenskiy's solution to determine the figure of the regularized geoid with a relative error on the order of the square of the earth's flattening. No need arises to determine the vertical gravity gradient. (Author) ; Trans. of Tsentralnyi Nauchno-Issledovatelskii Institut Geodezii, Aerosemki i Kartografii. Trudy (USSR) n176 p9-14 1969, by John M. Willis. Keyword: (*GEODESICS; *GEOIDS; *GRAVIMETRIC GEODESY; ANOMALIES; BOUNDARY VALUE PROBLEMS); DEFLECTION; EARTH(PLANET); ELLIPSOIDS; ERRORS; Geodesy; GRAVITY; NUMERICAL INTEGRATION; SPHERES; TRANSLATIONS; USSR URL: http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697627 http://www.dtic.mil/docs/citations/AD0697627 BASE Hide details

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