DIMENSION OF THE EARTH'S MEAN ELLIPSOID SPECIFIED BY BROVAR'S MODIFIED CONDITIONS. IN MEMORY OF PROFESSOR V V BROVAR

dc.contributor.author	Burša M.
dc.contributor.author	Šíma Z.
dc.contributor.author	Kouba J.
dc.contributor.author	Vatrt V.
dc.contributor.author	Yurkina M.I.
dc.date.accessioned	2022-08-15T01:48:52Z
dc.date.available	2022-08-15T01:48:52Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13472800
dc.identifier.citation	Acta Geodaetica et Geophysica Hungarica, 2004, 39, 1, 15-25
dc.identifier.issn	1217-8977
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38557
dc.description.abstract	The Brovar’s condition of minimizing the Earth’s anomalous gravity field focused to the determination of the parameters of the Earth’s mean ellipsoid has been discussed and applied in two modified and simplified versions. The condition $\int_{{S_0}} {{T^2}d{S_0}}$ = minimum has been applied over the world ocean area S 0 with the use of TOPEX/POSEIDON altimetry and mean sea surface topography height data. The semimajor axis of the Earth’s mean ellipsoid has been determined as a = (6 378 135.1 ± 1.5) m.
dc.title	DIMENSION OF THE EARTH'S MEAN ELLIPSOID SPECIFIED BY BROVAR'S MODIFIED CONDITIONS. IN MEMORY OF PROFESSOR V V BROVAR
dc.type	Статья

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