Simulating the Wave-Enhanced Layer under Breaking Surface Waves with Two-Equation Turbulence Models
By H. Burchard. 2001
143 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Oceanography
View Paper: https://www.semanticscholar.org/paper/fb7a51484f075099aa7e3dc5afb56ba5c9d4fc6b
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Fabrice Ardhuin
- Nicolas Rascle
- Y. Noh
- Jean-Raymond Bidlot
- H. Min
- Kristian Mogensen
- M. Balmaseda
- O. Breivik
In Earth-Surface Processes
- Nicolas Rascle
- Fabrice Ardhuin
- D. Croizé-Fillon
- Jean-Raymond Bidlot
- O. Breivik
- Kristian Mogensen
- M. Balmaseda
- Pierre Queffeulou
In Oceanography
- Fabrice Ardhuin
- Nicolas Rascle
- D. Croizé-Fillon
- Jean-Raymond Bidlot
- Kristian Mogensen
- M. Balmaseda
- Pierre Queffeulou
- O. Breivik
Citations in the corpus
- Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, background): “…in a number of single-column mixed-layer model experiments (Craig and Banner , 1994; McWilliams and Restrepo, 1999;McWilliams and Sullivan, 2000; Burchard , 2001;Kantha and Clayson, 2004;Mellor and Blumberg, 2004; Rascle et al., 2006; Ardhuin and Jenkins, 2006; Huang et al., 2011; Janssen,…”
- Wave Breaking and Ocean Surface Layer Thermal Response (2004, unknown): “Burchard (2001) made a fairly complicated alteration to the k– model [which now includes Eq.”
- LARGE EDDY SIMULATION OF THE OCEAN MIXED LAYER: THE EFFECTS OF WAVE BREAKING AND LANGMUIR CIRCULATION (2004, background): “…efforts have been made to incorporate these effects into the ocean mixed layer models; for example, Noh and Kim (1999), D’Alessio et al. (1998), and Burchard (2001) for the effects of wave breaking and Li and Garrett (1997), D’Alessio et al. (1998), and McWilliams and Sullivan (2000) for the…”
- A global wave parameter database for geophysical applications. Part 1: Wave-current turbulence interaction parameters for the open ocean based on traditional parameterizations (2008, background): “…TKE surface flux Uoc coming from the dissipation of surface waves and by setting the near-surface mixing length at the surface z0 to a relatively large value, of the order of the f significant wave height Hs (Craig and Banner, 1994; Terray et al., 1996; Burchard, 2001; Acreman and Jeffery, 2007).”
- Wave-Current Interaction in an Oceanic Circulation Model with a Vortex-Force Formalism: Application to the Surf Zone (2010, unknown): “, Burchard (2001) has Kv decrease as z ? f , while Jones and Monismith (2008) has increase.”