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2 edition of Reducing the error of geoid undulation computations by modifying Stokes" Function. found in the catalog.

Reducing the error of geoid undulation computations by modifying Stokes" Function.

Christopher Jekeli

Reducing the error of geoid undulation computations by modifying Stokes" Function.

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Published by Ohio State University, Department of Geodetic Science in Columbus, Ohio .
Written in English


Edition Notes

SeriesReports / Department of Geodetic Science, Ohio State University -- no.301, Reports -- no.301.
The Physical Object
Paginationv, 50p. :
Number of Pages50
ID Numbers
Open LibraryOL13791412M


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Reducing the error of geoid undulation computations by modifying Stokes" Function. by Christopher Jekeli Download PDF EPUB FB2

Author of Alternative methods to smooth the earth's gravity field, The downward continuation to the earth's surface of truncated spherical and ellipsoidal harmonic series of the gravity and height anomalies, Global accuracy estimates of point and mean undulation differences obtained from gravity disturbances, gravity anomalies and potential coefficients, An investigation of two models for the.

Šprlák M () Generalized geoidal estimators for deterministic modifications of spherical Stokes’ function. Contrib Geophys Geod 40(1)–64 CrossRef Reducing the error of geoid undulation computations by modifying Stokes Function.

book Scholar Tikhonov A () Solution of incorrectly formulated problems and the regularization by: 1. Stokes' integral, representing a surface integral from the product of terrestrial gravity data and spherical Stokes' function, is the theoretical basis for the modelling of the local geoid. Geoid determination utilizes gravity data collected on the Earth’s surface and its vicinity to compute the geoid in the most rigorous way.

To distinguish from global geoid determination which requires global data coverage, local geoid determination focuses only on local areas or regions. Regional geoid computations are often based on numerical integration of gravity anomalies using modified Stokes's integration where Stokes's integral is evaluated with some kernel modification (e Author: Artu Ellmann.

verification of gravimetric geoidal models by a combination of gps and orthometric heights g. robinson may technical report no. Full text of "Satellite Altimetry for Geodesy, Geophysics and Oceanography [electronic resource]: Proceedings of the International Workshop on Satellite Altimetry, a joint workshop of IAG Section III Special Study Group SSG and IAG Section II, September.

POSTER’SESSION’ Session1:’Paleosealevel’dataandGIA’modelling ’ ’ Paper&ID&& Poster&BoardN°27& Geophysical&ModelingResultsand. Normal-mode Q as a function of angular degree / and overtone number n Reducing the error of geoid undulation computations by modifying Stokes Function.

book the spheroidal simple (a. c, e) and generalized (b, d, f) Burgers body rheologies for radial (,So), (J) and toroidal (J,) modes, respectively., DYNAMICS OF THE ICE AGE EARTH Reducing the error of geoid undulation computations by modifying Stokes Function.

book actenstic of Cited by: Remote Sensing Applications Compiled and Edited by Dr. Roy, Deputy Director, Remote Sensing & GIS Applications Area, NRSC Dr. R.S. Dwivedi and n RS & GIS Applications Area, NRSC Published by National Remote Sensing Centre Indian Space Research Organisation Dept.

of Space, Govt. of India, Balanagar, Hyderabad – The methodology followed, from the identification of the significant non-dimensional parameters that define the problem, the formulation of a zonal prediction model, a parametric numerical study by means of detailed multidimensional CFD computations and the post-processing of the results in order to feed the global model are exposed in detail.

The Geoid The level surface that corresponds to the surface of an ocean at rest is a special surface, the geoid. To a first approximation, the geoid is an ellipsoid that corresponds to the surface of a rotating, homogeneous fluid in solid-body rotation, which means that the fluid has no internal flow.

THE PHYSICAL SETTING The Geoid The level surface that corresponds to the surface of an ocean at rest is a special surface, the geoid. To a rst approximation, the geoid is an ellipsoid that corresponds to the surface of a rotating, homogeneous uid in solid-body rotation, which means that.

Using GPS and leveling data in local precise geoid determination and case study. NASA Astrophysics Data System (ADS) Erol, B.; Çelik, R. N.; Erol, S. the fundamental. Rep Geol Surv Jpn –28Sjöberg LE () A general model of modifying Stokes’ formula and its least squares solution.

J Geodesy – https:// doi. org/ / s CrossrefSmith DA, Roman DR () GEOID99 and G99SSS: 1-arc-minute geoid models for the United States.

J Geodesy 75(9–10)– The 5'×5' global geoid model GGM NASA Astrophysics Data System (ADS) Shen, WenBin; Han, Jiancheng. We provide an updated 5'×5' global geoid model GGM, which is determined based on the shallow layer method (Shen ).

We choose an inner surface S below the EGM geoid, and the layer bounded by the inner surface S and the Earth's geographical surface. The local geoid model is compared with a regional geoid undulation model and the results presented in table The creation of a Local Geoidal Undulation Model (LGUM) is justified since it provides a much better precision on the final results.

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Scribd is the world's largest social reading and publishing site. Search Search5/5(1). It presupposes the rotation invariance of the auto-correlation function, from which follows the rotation invariance of the auto-correlation function for the potential and again the rotation invariance for the domain of definition of the potential itself, independent of the way it is calculated: from Moritz’ formula and Stokes’ formula, or.

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