Pregled bibliografske jedinice broj: 1037129
The Geomed2 project: the Geoid and DOT of the Mediterranean Sea
The Geomed2 project: the Geoid and DOT of the Mediterranean Sea // ESA LP 2019 Abstracts
Milano, Italija, 2019. (poster, međunarodna recenzija, prošireni sažetak, znanstveni)
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Naslov
The Geomed2 project: the Geoid and DOT of the Mediterranean Sea
Autori
Barzaghi, Ricardo ; Vergos, Georgios S. ; Carrion, Daniela ; Albertella, Alberta ; Tziavos, Ilias N. ; Grigoriadis, Vassilios ; Natsiopoulos, Dimitrios ; Bruinsma, Sean ; Bonvalot, Sylvain ; Seoane, Lucia ; Reinquin, Frank ; Lequentrec-Lalancette, M-F ; Salaun, Corinne ; Bonnefond, Pascal ; Knudsen, P. ; Andersen, Ole ; Simav, Mehmet ; Yildiz, Hasan ; Bašić, Tomislav ; Varga, Matej ; Gil, A.J.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, prošireni sažetak, znanstveni
Izvornik
ESA LP 2019 Abstracts
/ - , 2019
Skup
ESA Living Planet Symposium
Mjesto i datum
Milano, Italija, 13.05.2019. - 17.05.2019
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Geoid ; Mediterranean Sea ; GEOMED
Sažetak
The main scope of the GEOMED2 project is the determination of a high-accuracy and high-resolution geoid and DOT models for the Mediterranean Sea. The processing methodology is based on the well-known remove-compute-restore procedure and both stochastic and integral/spectral methods for the determination of the geoid and the rigorous combination of heterogeneous data. All the available gravity observations for the wider Mediterranean basin were collected, validated, homogenized and unified in terms of their horizontal coordinates and gravity systems, so as to derive a reliable gravity data base to be used for the determination of the geoid. Particularly, marine gravity were track by track debiased in order to remove existing inconsistencies among the different gravity campaigns. Base on the collected data, the geoid has been computed in the wider Mediterranean area, i.e. in the area bounded between 30° < φ < 48° -10° < λ < 40°. The available gravity data have been gridded on a regular 2’ x 2’ grid in the computation area employing ordinary kriging, servicing both as input to the geoid estimation methodologies and as a project deliverable to be disseminated as a new approximation of the gravity field over the Mediterranean. Fast-collocation, 1dFFT and 2dFFT employing the original Wong-Gore modified Stokes kernel and the KTH methods have been applied in order to get the geoid estimate. The different geoid estimates have been then compared with altimeter data to obtain different estimates of the Dynamic Ocean Topography (DOT), which will allow the definition of the currents pattern in the Mediterranean Sea.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika, Geodezija
POVEZANOST RADA
Ustanove:
Geodetski fakultet, Zagreb