On the Interaction of Surface Waves and Upper Ocean Turbulence

By Fabrice Ardhuin, A. Jenkins. 2006

156 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/44aee8393fee8f5f6d22b1032b6b18aec183dd59

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

In Oceanography

Citations in the corpus

Observation of swell dissipation across oceans (2008, background): “Interaction with oceanic turbulence is expected to be relatively small [Ardhuin and Jenkins, 2006].”
Monitoring and analysis of ocean swell fields from space: New methods for routine observations (2009, background): “Furthermore, the level of turbulence in the ocean does not appear to significantly affect the waves [Fabrikant and Raevsky, 1994; Ardhuin and Jenkins, 2006], and the conversion of surface wave energy into internal gravity wave energy by wave-wave interactions does not seem to be a leading order…”
User manual and system documentation of WAVEWATCH III R version 4.18 (2014, methodology): “Finally, the wave-turbulence interaction term of Teixeira and Belcher (2002) and Ardhuin and Jenkins (2006), is given by”
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): “The processes that cause the swell attenuation are not fully elucidated (Ardhuin and Jenkins, 2006; WISE Group, 2007), but they are likely dominated by the damping of waves due to the strong shears at the air-sea interface (Weber and Førland, 1990; Kudryavtsev and Makin, 2004), resulting in a wave-d”
On a wave‐induced turbulence and a wave‐mixed upper ocean layer (2006, background): “…above, though), the latter feature of irrotationality imposes a serious limitation on the wave motion because it basically bans thewave-induced turbulence (although some theoretical mechanisms of generating the turbulence by irrotational waves are still possible [e.g., Ardhuin and Jenkins, 2006]).”
Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, background): “gniﬁcantly (Craig and Banner, 1994; Craig, 1996). Waves absorb energy and momentum from the wind ﬁeld when they grow and in turn release it when they break (Janssen et al., 2004; Rascle et al., 2006; Ardhuin and Jenkins, 2006; Janssen, 2012). This lowers or raises the stress on the water side (i.e.,”
On the Existence of Water Turbulence Induced by Nonbreaking Surface Waves (2009, background): “It should also be pointed out that such turbulence production cannot be attributed to Ardhuin and Jenkins (2006) or to similar mechanisms of wave–current–turbulence interactions.”
Surface gravity wave effects in the oceanic boundary layer: large-eddy simulation with vortex force and stochastic breakers (2007, background): “Craig & Banner 1994; McWilliams & Sullivan 2000; Smyth et al. 2002; Kantha & Clayson 2004; Lewis & Belcher 2004; Melsom & SAEtra 2004; Ardhuin & Jenkins 2006; Rascale, Ardhuin & Terray 2006), with improvements motivated by better measurements and results from turbulence-resolving simulations with ”