Wave capture and wave–vortex duality

By O. Bühler, M. McIntyre. Journal of Fluid Mechanics, 2005

229 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science

View Paper: https://www.semanticscholar.org/paper/e4ee07dee7b028d90acb1ed522b39818ae823ee1

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Citations in the corpus

Internal gravity waves from atmospheric jets and fronts (2014, background): “packets propagating through them has been emphasized in theoretical studies as wave-capture [Badulin and Shrira, 1993; Bühler and McIntyre, 2005].”
Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks (2009, background): “Müller (1976), and more recently Bühler and McIntyre (2005), showed that the deformations of internal wave packets propagating through the strain due to eddies result in an irreversible extraction of energy from the geostrophic field.”
TOWARD REGIONAL CHARACTERIZATIONS OF THE OCEANIC INTERNAL WAVEFIELD (2010, methodology): “In the limit of an extreme scale separation between wave and background flow, horizontal group velocities are small and an internal wave haves much like a passive tracer, [Bühler and McIntyre, 2005; Polzin, 2008a] as the rate of strain cascades the wave to higher horizontal wavenumber. As it does so”
Inertia–Gravity Waves Spontaneously Generated by Jets and Fronts. Part I: Different Baroclinic Life Cycles (2007, background): “Plougonven and Snyder (2005) argued that this can be due to propagation effects (wave capture; Bühler and McIntyre 2005) that are well described even at low resolution.”
Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Application to the Southern Ocean (2010, background): “Another direction for future research, discussed to some extent in the literature (Buhler and McIntyre 2005; Dewar and Killworth 1995; Polzin 2008) is to study the degree to which wave radiation extracts energy from the geostrophic eddy field.”
Submesoscale Processes and Dynamics (2013, background): “…shown whether this breakdown in balance leads to triggering energy into internal gravity waves, or whether direct interactions between the balanced submesoscale flows and a prexisting internal wave field affects energy transfer from large to small scales [Bühler and McIntyre, 2005; Polzin, 2006].”
Mean and variable forcing of the middle atmosphere by gravity waves (2006, background): “One additional caveat that is important to note is the requirement that the time scale for initial GW propagation, essentially its period, be shorter than the time scale of the radiated GWs, for the same reasons as discussed for adjustment processes above (Bühler and McIntyre, 2005).”
Submesoscale currents in the ocean (2016, background): “IGWs [99] and provide catalytic interactions that enhance the IGW forward energy cascade [81] (also related to ‘wave capture’ [100]), and lee IGWs can be generated by eddy currents over topography [52] (e.”
Eddy stirring in the Southern Ocean (2011, unknown): “The behavior of linear waves in non‐parallel, horizontally non‐ divergent background flows is, in the limit of an extreme scale separation between the waves and the background, analogous to that of passive scalars [Bühler and McIntyre, 2005; Polzin, 2008].”