The accuracy of surface elevations in forward global barotropic and baroclinic tide models
By B. Arbic, S. Garner, Robert Hallberg, H. Simmons. 2004
188 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/a56462e3abaa36330ee8167814f66dba31a13948
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In Global and Planetary Change
- S. Jayne
- Jonas Nycander
- G. Flierl
- S. Garner
- B. Arbic
- Raffaele Ferrari
- M. Nikurashin
- Oliver B. Fringer
In Oceanography
Citations in the corpus
- Generation of internal waves in the deep ocean by tides (2005, methodology): “They found theenergyflux tointernal waves inthe Pacific tobe 0.34 TW. [7] Very recently, Egbert et al. [2004] and Arbic et al. [2004] haveperformedcomputationsoftheenergyfluxbased on the linear wave theory developed by Bell [1975a, 1975b] and Llewellyn Smith and Young [2002].”
- Concurrent Simulation of the Eddying General Circulation and Tides in a Global Ocean Model (2010, unknown): “In contrast to earlier high-resolution global baroclinic tide simulations, which utilized tidal forcing only, the simulation presented here has a horizontally non-uniform stratification, supported by the wind- and buoyancy forcing.”
- The Impact of Abyssal Mixing Parameterizations in an Ocean General Circulation Model (2009, methodology): “Additionally, the gravitational self-attraction and loading term in the tidal model has been implemented using an iterative method (Egbert et al. 2004; Arbic et al. 2004).”
- Baroclinically Unstable Geostrophic Turbulence in the Limits of Strong and Weak Bottom Ekman Friction: Application to Midocean Eddies (2004, background): “Recent forward models of tides (Jayne and St. Laurent 2001; Arbic et al. 2004) parameterize the topographic drag and find that it must be quite strong to accurately simulate open-ocean tidal elevations.”
- A Topographic Drag Closure Built on an Analytical Base Flux (2005, background): “This result is directly relevant to internal waves generated by semidiurnal or higher-frequency tidal flows in the ocean (Arbic et al. 2004).”