Balance and Spontaneous Wave Generation in Geophysical Flows

163 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Submesoscale currents in the ocean (2016, background): “Unlike GI and CI, AAI does not have a sharp onset condition in a general fluid model, but rather can exhibit an exponentially small unstable growth rate, σ ∼ |∇u| exp[−C/Ro ] as Ro→ 0, which is also relevant to the asymptotic fuzziness of the slow (momentum-balanced) manifold (§4b; [10]), but with σ”
Internal gravity waves from atmospheric jets and fronts (2014, background): “Several lines of evidence have progressively shown that such emission is inevitable, i.e., that an exactly invariant slow manifold in fact does not exist and that one should rather think of slow manifolds of various accuracies [MacKay, 2004; Vanneste, 2013, and references therein].”
Review of wave‐turbulence interactions in the stable atmospheric boundary layer (2015, background): “…Luo, 1992; Fritts and Alexander, 2003], atmospheric jets and fronts [e.g., Mastrantonio et al., 1976; Chimonas and Grant, 1984; Plougonven and Zhang, 2014], or the spontaneous loss of balanced motions [e.g., Vanneste, 2013], but we do consider higher-frequency waves resulting from these processes.”