EGM08 and local quasigeoid model in Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025615%3A_____%2F09%3A%230001622" target="_blank" >RIV/00025615:_____/09:#0001622 - 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

EGM08 and local quasigeoid model in Czech Republic

Popis výsledku v původním jazyce

Presentation on the EGU General Assembly, Vienna, April 2009. Abstract: Two quasigeoid models are tested at over 1000 points, where both normal and ellipsoidal heights are known,in a test area in the Czech Republic: a global model computed from EGM08 anda combined model containingboth long-wavelength part from EGM08 and short-wavelength part from local terrestrial gravity measurements.Although the new EGM08 was used up to degree and order 2160, the short-wavelength part of quasigeoid generatedby residual anomalies still riches values up to 14 cm. However, the short-wavelength part of quasigeoid is notimproving the quasigeoid model at some zones of the test area. These errors in short-wavelength part of quasigeoidare probably caused by systematic errors in local gravity or height data.

Název v anglickém jazyce

EGM08 and local quasigeoid model in Czech Republic

Popis výsledku anglicky

Presentation on the EGU General Assembly, Vienna, April 2009. Abstract: Two quasigeoid models are tested at over 1000 points, where both normal and ellipsoidal heights are known,in a test area in the Czech Republic: a global model computed from EGM08 anda combined model containingboth long-wavelength part from EGM08 and short-wavelength part from local terrestrial gravity measurements.Although the new EGM08 was used up to degree and order 2160, the short-wavelength part of quasigeoid generatedby residual anomalies still riches values up to 14 cm. However, the short-wavelength part of quasigeoid is notimproving the quasigeoid model at some zones of the test area. These errors in short-wavelength part of quasigeoidare probably caused by systematic errors in local gravity or height data.

Druh

O - Ostatní výsledky

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/2C06028" target="_blank" >2C06028: Tvorba znalostního systému pro podporu rozhodování založeného na geodatech</a><br>

Návaznosti

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

Rok uplatnění

2009

Kód důvěrnosti údajů

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