On the distortion of turbulence by a progressive surface wave

By Miguel C. Teixeira, S. Belcher. Journal of Fluid Mechanics, 2002

210 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/c216127cae5d57bf9fa09307f3f903280ab8260d

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Citations in the corpus

The Role of Wave-Induced Coriolis–Stokes Forcing on the Wind-Driven Mixed Layer (2005, background): “Distortion of turbulent vorticity by Stokes drift is at the heart of models for Langmuir circulations (Leibovich 1983; McWilliams et al. 1997; Teixeira and Belcher 2002).”
Explicit wave-averaged primitive equations using a generalized Lagrangian mean (2007, methodology): “This is usual practice in air-sea interaction studies, and it has provided approximate solutions to problems such as wind-wave generation or wave-turbulence interactions (e.g. Jenkins 1986, Teixeira and Belcher 2002) but it brings some complications.”
Numerical modeling of ocean swell contributions to the global wind-wave climate (2006, methodology): “Winds from the GFS are reduced from the model s lowest vertical level (995 mB or 35 m) to the standard 10-m height assuming neutral stability, as described in Tolman (1998a).”
User manual and system documentation of WAVEWATCH III R version 4.18 (2014, methodology): “Details on the management algorithm developed to run all grid simultaneously can be found in Tolman (2007, section 3.4) or Tolman (2008a), and will not be reproduced here.”
Challenges and Prospects in Ocean Circulation Models (2019, background): “The theoretical underpinnings of this idea extend back to Langmuir (1938), but modern theory (Craik and Leibovich, 1976; Teixeira and Belcher, 2002), modeling (Denbo and Skyllingstad, 1996; McWilliams et al.”
Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, background): “…eddy simulations (LES) to investigate the impact of Langmuir turbulence in the upper ocean (Skyllingstad and Denbo, 1995; McWilliams et al., 1997; Teixeira and Belcher , 2002; Polton and Belcher , 2007;Grant and Belcher , 2009), and in some cases even direct numerical simulations (DNS) have been…”
A global perspective on Langmuir turbulence in the ocean surface boundary layer (2012, unknown): “Stokes drift deforms absolute vorticity into the horizontal generating streamwise vortices of Langmuir turbulence [Craik and Leibovich, 1976; Teixeira and Belcher, 2002].”
Characteristics of Langmuir Turbulence in the Ocean Mixed Layer (2009, background): “Linear vorticity dynamics in rapid distortion theory captures these differences (Teixeira and Belcher 2002).”
On the Interaction of Surface Waves and Upper Ocean Turbulence (2006, methodology): “ Teixeira and Belcher (2002) instead considered the evolution of Reynolds stresses”