Differential geometry of equipotential surfaces and its relation to parameters of Earth?s gravity field models

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025615%3A_____%2F15%3A%230002198" target="_blank" >RIV/00025615:_____/15:#0002198 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Differential geometry of equipotential surfaces and its relation to parameters of Earth?s gravity field models

Popis výsledku v původním jazyce

According to adopted conventions the notion of an equipotential surface of the Earth?s gravity potential is of key importance for vertical datum definition. The aim of this contribution is to focus on differential geometry properties of equipotential surfaces and their relation to parameters of Earth?s gravity field models. Within this concept one can apply a number of tools. The discussion mainly rests on the use of Weingarten?s theorem that has an important role in the theory of surfaces and in parallel an essential tie to Brun?s equation (for gravity gradient) well known in physical geodesy. Also Christoffel?s theorem and its use will be mentioned. These considerations are of constructive nature and numerically their content will be demonstrated forhigh degree and order gravity field models. The results will be interpreted globally and also in merging segments expressing regional and local features of the gravity field of the Earth. They may contribute to the knowledge important fo

Název v anglickém jazyce

Differential geometry of equipotential surfaces and its relation to parameters of Earth?s gravity field models

Popis výsledku anglicky

According to adopted conventions the notion of an equipotential surface of the Earth?s gravity potential is of key importance for vertical datum definition. The aim of this contribution is to focus on differential geometry properties of equipotential surfaces and their relation to parameters of Earth?s gravity field models. Within this concept one can apply a number of tools. The discussion mainly rests on the use of Weingarten?s theorem that has an important role in the theory of surfaces and in parallel an essential tie to Brun?s equation (for gravity gradient) well known in physical geodesy. Also Christoffel?s theorem and its use will be mentioned. These considerations are of constructive nature and numerically their content will be demonstrated forhigh degree and order gravity field models. The results will be interpreted globally and also in merging segments expressing regional and local features of the gravity field of the Earth. They may contribute to the knowledge important fo

Druh

A - Audiovizuální tvorba

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/GA14-34595S" target="_blank" >GA14-34595S: Matematické metody pro studium tíhového pole Země</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

ISBN

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Místo vydání

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Název nakladatele resp. objednatele

International Union of Geodesy and Geophysics

Verze

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Identifikační číslo nosiče

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