On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025615%3A_____%2F12%3A%230001837" target="_blank" >RIV/00025615:_____/12:#0001837 - isvavai.cz</a>
Výsledek na webu
—
DOI - Digital Object Identifier
—
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth
Popis výsledku v původním jazyce
Global models of the gravity field of the Earth that involve terrestrial measurements and GOCE-based gravity field models represent two different sources of information on the gravity field of the Earth. The aim of this paper is to focus on their combination. The problem has an essential tie to potential theory and it is not difficult to realize that by nature it is an overdetermined problem. Therefore, methods typical for the solution of boundary-value problems of potential theory will be applied together with an optimization approach, target function and regularization techniques. The aim also is to demonstrate the effect of the two different data sources on the resulting solution and to show its spectral and space domain interpretation. In particular, the use of gravity field information contained in satellite-only models of the gravity field of the Earth or alternatively in GOCE gradiometric data in common with terrestrial gravity measurements is discussed in the paper. The compati
Název v anglickém jazyce
On the differences and compatibility of global and GOCE-based models of the gravity field of the Earth
Popis výsledku anglicky
Global models of the gravity field of the Earth that involve terrestrial measurements and GOCE-based gravity field models represent two different sources of information on the gravity field of the Earth. The aim of this paper is to focus on their combination. The problem has an essential tie to potential theory and it is not difficult to realize that by nature it is an overdetermined problem. Therefore, methods typical for the solution of boundary-value problems of potential theory will be applied together with an optimization approach, target function and regularization techniques. The aim also is to demonstrate the effect of the two different data sources on the resulting solution and to show its spectral and space domain interpretation. In particular, the use of gravity field information contained in satellite-only models of the gravity field of the Earth or alternatively in GOCE gradiometric data in common with terrestrial gravity measurements is discussed in the paper. The compati
Klasifikace
Druh
A - Audiovizuální tvorba
CEP obor
DE - Zemský magnetismus, geodesie, geografie
OECD FORD obor
—
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2012
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
ISBN
—
Místo vydání
Vienna
Název nakladatele resp. objednatele
European Geoscience Union
Verze
—
Identifikační číslo nosiče
—