Results 91 to 100 of about 1,485 (143)
Autofrecuencias del movimiento del polo para un modelo de tierra de tipo Jeffreys-Molodensky.
Antonio G. Camacho, Miguel J. Sevilla
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80 years of Molodensky`s theory
The article deals with Mikhail Sergeyevich Molodensky, the USSR Science Academy Corresponding Member’s heritage part concerning to the main task of higher geodesy - determining the Earth’s physical surface and the external gravitational field.
V. Popadyev
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Molodensky Seven Parameter Transformation for Precise Urban Mapping
The existing coordinate system for the entire country of Ecuador is the Provisional South American Datum of 1956 (PSAD56) which originated in La Canoa, Venezuela. This coordinate system is considered one of the major datums of the world and is generally associated with the countries of South America that comprise the Andes Mountain Range. The system is
Javier Urquizo, C. Mugnier
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Numerical solution of the Molodensky boundary value problem with a fixed boundary
The functions of modern global navigation satellite systems (GNSS) allow us to consider the Earth’s surface as partially known at least. So, you can directly use the results of measurements on the real Earth surface, which significantly simplifies the ...
Yu.M. Neiman +2 more
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General inverse of Stokes, Vening-Meinesz and Molodensky formulae
The operator operations between the disturbing potential and the geoidal undulation, the gravity anomaly, the deflection of the vertical are defined based on the relations among the gravity potential, the normal gravity potential and the disturbing potential.
Cheng Luying, Xu Houze
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On the Equivalent Linearized BVP’s of Molodensky and Helmert
The two approaches, Molodensky and Helmert, are proved to be equivalent at the level of formulation of the linearized GBVP, according to the definitions introduced in Chap. 2.
F. Sansò, M. Sideris
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Advances in the numerical solution of the linear molodensky problem
The solution of the linear Molodensky problem by analytical continuation to point level is numerically the most convenient of all the theoretically equivalent solutions. It is obtained by successively applying the same integral operator and it does not depend explicitly on the terrain inclination.
M. Sideris, K. Schwarz
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Michael Sergeevich Molodensky (to the 100 anniversary)
A. Kozenko
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The Observation Equation of Spirit Leveling in Molodensky's Context
, 2015Spirit leveling and surface gravity observations can be expressed as orthometric height differences plus corrections which require the knowledge of the Earth crust density. For leveling increments we can write observation equations in a linearized form, according to the standard Molodensky approach, i.e., intrinsic geodesy, depending on normal height ...
B. Betti +3 more
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