Waves and Mean Flows

By O. Bühler. 2009

312 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/b56139d0cc08ec3bd79988a13c57782e1feff36a

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Citations in the corpus

The deep propagating gravity wave experiment (deepwave): an airborne and ground-based exploration of gravity wave propagation and effects from their sources throughout the lower and middle atmosphere (2016, background): “…mean flow interactions, and responses (Lindzen and Holton 1968; Holton 1982; Garcia and Solomon 1985; Haynes et al. 1991; Sutherland 2010; Bühler 2014); 4) GW spectral properties, interactions, instabilities, and saturation (Yeh and Liu 1981; Smith et al. 1987; Hines 1991; Lombard and…”
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Application to the Southern Ocean (2010, background): “The IOs provide a background shear that promotes wave breaking so that a large fraction of the internal wave pseudomomentum (Bühler 2009) is deposited where the E–”
The dynamics of waves interacting with the Equatorial Undercurrent (2015, background): “These can trigger instabilities in marginally stable flows, and they are places where momentum and energy exchange between the waves and the mean flow can occur (see the discussion in Bühler (2009), Haynes (2003)); the evidence is accumulating as to their appearance and importance in EUC-type flows.”
Internal gravity waves from atmospheric jets and fronts (2014, background): “This warrants an analogy [Bühler, 2009] between the evolution equation for the wave vector and for the evolution of the gradient of a passive, conserved tracer 𝜙, respectively: d𝐤 dt = − (∇𝐔) ⋅ 𝐤 and D∇𝜙 Dt = − (∇𝐔) ⋅ ∇𝜙 , (7) where the first equation may be written with indicial notation as…”
A Framework for Parameterizing Eddy Potential Vorticity Fluxes (2012, unknown): “Alternatively, to the extent that the eddies can be modeled as linear waves, one might use ray-tracing theory (e.g., Bühler 2009) to determine how the eddies are deformed by the background shear.”