An exact solution for equatorial geophysical water waves with an underlying current
By David Henry. 2013
198 citations recorded by the source corpus.
Abstract In this paper we present an exact solution to the governing equations for equatorial geophysical water waves which admit an underlying current.
Subfields: Atmospheric Science, Oceanography
View Paper: https://www.semanticscholar.org/paper/11d1a4115c32898c870a83f382c1e8a07075dceb
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In Atmospheric Science
In Oceanography
Citations in the corpus
- An Exact, Steady, Purely Azimuthal Flow as a Model for the Antarctic Circumpolar Current (2016, background): “approximation close to a fixed latitude (as in Pollard 1970; Mollo-Christensen 1979) or, for equatorial flows, the b-plane approximation (see Constantin 2012, 2014; Henry 2013; Hsu 2014; Ionescu-Kruse 2015).”
- The dynamics of waves interacting with the Equatorial Undercurrent (2015, methodology): “For a meridional width of 300 km, the values (38) predict a mass transport of about 40 Sv (1 Sv = 106 m3 s−1), thus corroborating the realistic nature of our model (see the field data in Izumo (2013)).”
- Some Nonlinear, Equatorially Trapped, Nonhydrostatic Internal Geophysical Waves (2014, background): “…periodic gravity water wave, where the particle paths are open loops in the absence of a current, and closed particle paths can only occur at a certain depth and only if there is a sufficiently strong adverse uniform current (see Constantin 2006; Henry 2008; Constantin and Strauss 2010).”
- An Exact, Steady, Purely Azimuthal Equatorial Flow with a Free Surface (2016, background): “A general introduction to these types of flows can be found in McCreary (1985), McPhaden et al.”