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Upper mantle temperatures illuminate the Iceland hotspot track and understanding of ice-Earth interactions in Greenland. [PDF]
Ajourlou P +10 more
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Vegetation cover fraction and the residential distribution of child-rearing households in urban Tokyo and Osaka: An ecological cross-sectional analysis. [PDF]
Otani M, Matsushita D.
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Prognostic Properties of Instantaneous Amplitudes Maxima of Earth Surface Tremor. [PDF]
Lyubushin A, Rodionov E.
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The Analysis of the Geodetic Boundary Value Problem: State and Perspectives
Geosystems Mathematics, 2018The geodetic boundary value problem is mathematically a freeboundary, oblique derivative boundary value problem for the Laplace operator. The solution of the problem is the determination of the shape of the Earth and of its gravity field. The analysis of such a problem, specially for its non-linear formulation, is hard, so it started only in 1976 with ...
Fernando Sanso, Sanso Fernando
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The solution of the general geodetic boundary value problem by least squares
Journal of Geodesy, 2001zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Rummel R, R Rummel
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Recent advances in the theory of the geodetic boundary value problem
Reviews of Geophysics, 1981After a short discussion on the general meaning of boundary value problems in physical geodesy the most classical Molodensky’s problem is considered. Recent advancements in the study of this problem, in both the classical and the gravity space approach, are discussed.
F. Sansò
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Bulletin Geodesique, 1985
Various formulations of the geodetic fixed and free boundary value problem are presented, depending upon the type of boundary data. For the free problem, boundary data of type astronomical latitude, astronomical longitude and a pair of the triplet potential, zero and first-order vertical gradient of gravity are presupposed.
E W Grafarend, B Heck, Heck B
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Various formulations of the geodetic fixed and free boundary value problem are presented, depending upon the type of boundary data. For the free problem, boundary data of type astronomical latitude, astronomical longitude and a pair of the triplet potential, zero and first-order vertical gradient of gravity are presupposed.
E W Grafarend, B Heck, Heck B
exaly +3 more sources
Solution of the geodetic boundary value problem for a reference ellipsoid
Journal of Geophysical Research, 1969The solution of the geodetic boundary value problem for a reference ellipsoid is given with a relative error of the order of the square of the earth's flattening. The solution is obtained by representing the disturbing potential at the earth's surface as the potential of a simple layer.
K. Koch
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