The Three-Dimensional Current and Surface Wave Equations
By G. Mellor. 2003
312 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Oceanography
View Paper: https://www.semanticscholar.org/paper/485ceb561ba1feaeb5aec76b7fcfcae7a19db8a3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Earth-Surface Processes
- Nicolas Rascle
- L. Umlauf
- Kostas Belibassakis
- John C. Warner
- Fabrice Ardhuin
- H. Burchard
- Courtney K. Harris
- Richard P. Signell
In Oceanography
- L. Umlauf
- Fabrice Ardhuin
- H. Burchard
- Nicolas Rascle
- Kostas Belibassakis
- John C. Warner
- Courtney K. Harris
- Richard P. Signell
Citations in the corpus
- Second-order turbulence closure models for geophysical boundary layers. A review of recent work (2005, background): “An interesting step into this direction has been suggested by Mellor (2003), who outlined the conceptual frame work for such models.”
- A global wave parameter database for geophysical applications. Part 1: Wave-current turbulence interaction parameters for the open ocean based on traditional parameterizations (2008, unknown): “The main difference with the model of Mellor and Yamada (1982) is that the flux Richardson number is replaced by a turbulent Richardson number, which is more convenient in the surface layer where the production of turbulence by the mean current shear is not the dominant source of TKE (Noh, 1996; Me”
- Explicit wave-averaged primitive equations using a generalized Lagrangian mean (2007, background): “Mellor (2003) following ξ3 total (uL) 2nd order, flat bottom”
- Wave-Current Interaction in an Oceanic Circulation Model with a Vortex-Force Formalism: Application to the Surf Zone (2010, unknown): “Accordingly,t is anticipated that the 3D737 radiation-stress model (e.g., Mellor, 2003) could have noticeable deficiency for surfzone applications.738 In addition, a more vertically-sheared velocity field with the appropriateBb forcing is essential to more739 correct VF representation that leads to…”
- Development of a three-dimensional, regional, coupled wave, current, and sediment-transport model (2008, methodology): “where the horizontal radiation-stress terms (Phillips, 1969; Mellor, 2003, 2005) with roller contributions based on Svendsen (1984) and Svendsen et al. (2002) are:”