Analysis of Quasi-Geoid Model Created for Territory of the Republic of Armenia

Venera Margaryan

doi:10.4028/www.scientific.net/AMR.1020.484

Paper Titles

Shaking Table Test Study on Seismic Responses of Base-Isolated Buildings under Near-Fault Ground Motions
p.457

Seismic Response of Underground Structure under Vertical Seismic Excitation
p.463

Basics of Metals Theory of Extraction by Means of Chemical Water Solutions Filtration through Underground Ores
p.472

Prediction of the Erosive Processes in the Corridor of Baku-Tbilisi-Ceyhan Oil Pipeline and Development of Methods to Design the New Engineering Environmental Protection Measures
p.478

Analysis of Quasi-Geoid Model Created for Territory of the Republic of Armenia
p.484

Economic Aspects of Implementing Energy Performance Labelling of Buildings and Flats in the Czech Republic
p.491

Microgeneration Based on Renewable Energy in Sustainable Building
p.495

Exploitation of Heat from Thermal Active Coal Tips
p.501

The Utilization of Ground Source Heat Pumps (GSHP) for Research Purpose in the Campus of VSB - Technical University of Ostrava
p.507

HomeAdvanced Materials ResearchAdvanced Materials Research Vol. 1020Analysis of Quasi-Geoid Model Created for...

Analysis of Quasi-Geoid Model Created for Territory of the Republic of Armenia

Abstract:

Abstract: National Geodesic Network of WGS-84 system was founded in the territory of the Republic of Armenia from 2002 to 2007, which includes zero, first, and second class 1115 stations and there were other 229 State Geodesic Triangular Network stations. The observation at these stations has been done by GPS system. Each of the above mentioned stations covers on the average 27 square kilometers of the territory of Armenia. The data obtained during GPS observations have become the foundation for creating local quasi-geoid models and obtaining differences of heights (geoid wave value) of normal and WGS-84 ellipsoid surfaces. On the basis of gravimetric data a quasi-geoid model has been computed and developed. To creat the model coordinates of four geodetic satations encompassing the area of the Republic of Armenia have been used. To get the digital model of the selected area was diveded into five-minute sections by latitude and longitude and then coordinates of geodetic points have been taken. The above mentioned points were recalculated from the local system to WGS-84 system. The creation of the local elippsoid quasi-model is conditioned by the difference of 3D coordinates difference of three-dimensional of each point’s position. The values of the geoid wave vary within the range of 17.4547 meters, the average difference being almost in the centre of the area and is 21.2522 meters. To obtain the digital model of the quasi-geoid at the given local ellipsoid at each 100m a square matrix (of the network) was made by coordinates of recomputed points.

You might also be interested in these eBooks

Contemporary Problems in Architecture and Construction

View Preview

Info:

Periodical:

Advanced Materials Research (Volume 1020)

Pages:

484-487

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.1020.484

Citation:

Cite this paper

Online since:

October 2014

Authors:

Venera Margaryan*

Keywords:

Coordinates, Model, Network, Quasi-Geoid, WGS-84 System

Export:

RIS, BibTeX

Price:

Permissions CCC:

Request Permissions

Permissions PLS:

Request Permissions

Сopyright:

Citation:

* - Corresponding Author

References

[1] O.S. Petrosyan, V.A. Margaryan, National Geodetic Network of RA., Proceedings of Higher Educational Institutions, Geodesy and Aerial Photography, № 6, Moscow, 2011, pp.27-32.

Google Scholar

[2] L.V. Manukyan, G.A. Aloyan. Characteristics of the Network of Permanently Acting Reference Stations Iimplementation in the Republic of Armenia. Bulletin of Builders Union of Armenia. N1-2, Yerevan 2011, pp.161-162.

Google Scholar

[3] M.S. Molodenski, Gravitational Field, Figure and Internal Structure of the Earth, Moscow, Nauka, 2001. p.569.

Google Scholar