Resení geoidu z leteckych tihovych dat

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F49777513%3A23520%2F03%3A00000395" target="_blank" >RIV/49777513:23520/03:00000395 - 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

The determination of the geoid from airborne gravity data

Popis výsledku v původním jazyce

The theory for the determination of the gravimetric geoid, i.e., the geoid based on worldwide observations of gravity, has been known for about 150 years (Stokes 1849). Its modification for the application of airborne gravimetry, i.e., for gravity observed from a low-altitude flying aircraft is the main topic of this report. The concept of a band-limited geoid is used in the following, i.e., of a geoid that is based on the band-limited frequency spectrum that can be resolved from discrete band-limited airborne gravity data in a certain geographically-limited area. Theoretical formulations of mathematical models are accompanied by derivations of practical computational formulae applicable for the determination of the gravimetric geoid. The solution is based on the combination of airborne gravity data with a global geopotential model.

Název v anglickém jazyce

The determination of the geoid from airborne gravity data

Popis výsledku anglicky

The theory for the determination of the gravimetric geoid, i.e., the geoid based on worldwide observations of gravity, has been known for about 150 years (Stokes 1849). Its modification for the application of airborne gravimetry, i.e., for gravity observed from a low-altitude flying aircraft is the main topic of this report. The concept of a band-limited geoid is used in the following, i.e., of a geoid that is based on the band-limited frequency spectrum that can be resolved from discrete band-limited airborne gravity data in a certain geographically-limited area. Theoretical formulations of mathematical models are accompanied by derivations of practical computational formulae applicable for the determination of the gravimetric geoid. The solution is based on the combination of airborne gravity data with a global geopotential model.

Druh

B - Odborná kniha

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2003

Kód důvěrnosti údajů

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

ISBN

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Počet stran knihy

1

Název nakladatele

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Místo vydání

Praha

Kód UT WoS knihy

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