Results 161 to 170 of about 159,970 (226)

Upper mantle temperatures illuminate the Iceland hotspot track and understanding of ice-Earth interactions in Greenland. [PDF]

open access: yesProc Natl Acad Sci U S A
Ajourlou P   +10 more
europepmc   +1 more source
Some of the next articles are maybe not open access.

Related searches:

The Analysis of the Geodetic Boundary Value Problem: State and Perspectives

Geosystems Mathematics, 2018
The 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
exaly   +3 more sources

The solution of the general geodetic boundary value problem by least squares

Journal of Geodesy, 2001
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Rummel R, R Rummel
exaly   +3 more sources

Recent advances in the theory of the geodetic boundary value problem

Reviews of Geophysics, 1981
After 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
exaly   +3 more sources

The free versus fixed geodetic boundary value problem for different combinations of geodetic observables

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
exaly   +3 more sources

Solution of the geodetic boundary value problem for a reference ellipsoid

Journal of Geophysical Research, 1969
The 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
openaire   +2 more sources

Home - About - Disclaimer - Privacy