The Interaction of Ocean Waves and Wind

By Peter A. E. M. Janssen. 2004

550 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Oceanography

View Paper: https://www.semanticscholar.org/paper/599b08fbb38c200aceb450b72a41ecf38843b1ae

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Citations in the corpus

Surface Wave Effects in the NEMO Ocean Model: Forced and Coupled Experiments (2015, methodology): “Third generation spectral wave models (Hasselmann et al., 1988; Tolman, 1991; Komen et al., 1994; Ris et al., 1999; Janssen, 2004; Tolman et al., 2002; Holthuijsen, 2007; Cavaleri et al., 2007) solve the action balance equation (see Eq (1.185) by Komen et al. (1994) and Eq (2.71) by Janssen (2004))…”
On the Interaction of Surface Waves and Upper Ocean Turbulence (2006, background): “In addition to interaction with the airflow that tends to dissipate waves traveling faster than the wind or against the wind (e.g., Kudryavtsev and Makin 2004), it has been suspected for a long time that waves interact with oceanic turbulence.”
Error Estimation of Buoy, Satellite, and Model Wave Height Data (2007, background): “A preliminary account of this work may be found in Janssen (2004).”
Projection of Global Wave Climate Change toward the End of the Twenty-First Century (2012, methodology): “…generated by a two-way coupled atmosphere–wave model systems, where wind fields and other atmospheric parameters that influence wave growth are passed to the wave model, which returns information about the impact of the sea state on surface roughness via the Charnok parameter (Janssen 1991, 2004).”
Climate model configurations of the ECMWF Integrated Forecasting System (ECMWF-IFS cycle 43r1) for HighResMIP (2018, methodology): “The ocean-wave model interacts with the atmosphere and oceans through exchange of the Charnock parameter that determines the sea surface roughness (Janssen, 2004) and by introducing a sea-state-dependent modification of the turbulent kinetic energy flux used for ocean mixing (Janssen et al., 2013;…”
Rogue waves and their generating mechanisms in different physical contexts (2013, background): “Oceanographers have historically treated the surfacewaves as a homogeneous and stationary stochastic processes characterized by Fourier phases uniformly distributed in the [0, 2π) interval, [21,22].”
Explicit wave-averaged primitive equations using a generalized Lagrangian mean (2007, background): “A proper closure involves a full discussion of the distortion of turbulence by the waves when the turbulent mixing time scale is larger than the wave period (e.g. Walmsley and Taylor 1996, Janssen 2004, Teixeira and Belcher 2002).”
Modeling hurricane waves and storm surge using integrally-coupled, scalable computations (2011, result): “The SI errors are large compared to other wave studies (Cardone et al., 1996; Janssen, 2004), but they reflect the complexities of modeling hurricane systems that change rapidly over multiple scales.”