Tide-surge, tide and surge simulations output of 2D DCSM-FM v7 from 1980 to 2020 at Euro platform. ...

This dataset includes results of hydrodynamic simulations for Euro platform, an offshore structure located in the southern North Sea that serves as a beacon for shipping and a measurement platform for the location. The results were generated with the 2D Dutch Continental Shelf Model - Flexible Mesh (DCSM, [Zijl and Groenenboom, 2019]), the successor of the version in Zijl et al. [2013,2015]. The model describes the tide-surge water level variability for the northwest European continental shelf between 15◦W to 13◦E and 43◦N to 64◦N by solving the depth-integrated shallow-water equations for hyd... Mehr ...

Verfasser: Guarneri, Henrique
Verlaan, M. Martin
Slobbe, D. C. Cornelis
Zijl, Firmijn
Klees, R. Roland
Pietrzak, J.D. Julie
Snellen, M. Mirjam
Keyzer, Lennart
Afrasteh, Yosra
Dokumenttyp: dataset
Erscheinungsdatum: 2022
Verlag/Hrsg.: 4TU.ResearchData
Schlagwörter: Oceanography / FOS: Earth and related environmental sciences / North Sea / Tides / tide-surge interaction / Europlatform / Dutch Continental Shelf Model v7 / Water Level / Time: 1980-2020
Sprache: unknown
Permalink: https://search.fid-benelux.de/Record/base-28980299
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : https://dx.doi.org/10.4121/21070933.v1

This dataset includes results of hydrodynamic simulations for Euro platform, an offshore structure located in the southern North Sea that serves as a beacon for shipping and a measurement platform for the location. The results were generated with the 2D Dutch Continental Shelf Model - Flexible Mesh (DCSM, [Zijl and Groenenboom, 2019]), the successor of the version in Zijl et al. [2013,2015]. The model describes the tide-surge water level variability for the northwest European continental shelf between 15◦W to 13◦E and 43◦N to 64◦N by solving the depth-integrated shallow-water equations for hydrodynamic modeling of free-surface flows [Leendertse, 1967, Stelling, 1984]. Water level conditions are applied at the northern, western, and southern open boundaries. When modeling the tide-surge water levels, they are composed of the sum of the astronomical water levels and the surge. The tides are obtained from a harmonic expansion of 32 tidal constituents retrieved from the global ocean tide model FES2012 [Carr`ere ...