Time-domain modeling of global ocean tides generated by the full lunisolar potential

Author:

Einšpigel DavidORCID,Martinec Zdeněk

Funder

European Space Agency (FR)

Ministerstvo Školství, Mládeže a Tělovýchovy (CZ)

Univerzita Karlova v Praze

Publisher

Springer Science and Business Media LLC

Subject

Oceanography

Reference71 articles.

1. Accad Y, Pekeris CL (1978) Solution of the tidal equations for the M 2 and S 2 tides in the world oceans from a knowledge of the tidal potential alone. Phil Trans R Soc A 290(1368):235–266

2. Agnew DC (2007) Earth tides. In: Treatise on Geophysics, Elsevier, pp 163–195

3. Amante C, Eakins BW (2009) ETOPO1 1 arc-minute global relief model: Procedures, data sources and analysis. NOAA Technical Memorandum NESDIS NGDC-24, p 19

4. Arakawa A, Lamb VL (1977) Computational design of the basic dynamical processes of the UCLA general circulation model. In: Chang J (ed) Methods in Computational Physics, Vol. 17, Academic Press, pp 174–265

5. Arbic BK, Garner ST, Hallberg RW, L SH (2004) The accuracy of surface elevations in forward global barotropic and baroclinic tide models. Deep-Sea Res II 51:3069–3101. doi: 10.1016/j.dsr2.2004.09.014

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