2014
DOI: 10.1088/0169-5983/46/3/031406
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A Lagrangian particle/panel method for the barotropic vorticity equations on a rotating sphere

Abstract: We present a Lagrangian particle/panel method for geophysical fluid flow described by the barotropic vorticity equations on a rotating sphere. The particles carry vorticity and the panels are used in discretizing the Biot-Savart integral for the velocity. Adaptive panel refinement and a new Lagrangian remeshing scheme are applied to reduce the computational cost and maintain accuracy as the flow evolves. Computed examples include a Rossby-Haurwitz wave, a Gaussian vortex, and a perturbed zonal jet. To validate… Show more

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Cited by 15 publications
(13 citation statements)
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“…Using this procedure he concluded that the emergent noise in his model was due to a small but significant divergence field missing from the initial fields. Even though the solutions of the non-divergent barotropic vorticity equation are not solutions of the shallow-water equations (SWEs), Phillips' procedure was adopted by Williamson et al (1992) as a standard test case for shallow-water models and has been extensively used ever since (Jablonowski et al, 2009;Mohammadian and Marshall, 2010;Bosler et al, 2014;Ullrich, 2014;Li et al, 2015, are only five recent examples).…”
Section: Introductionmentioning
confidence: 99%
“…Using this procedure he concluded that the emergent noise in his model was due to a small but significant divergence field missing from the initial fields. Even though the solutions of the non-divergent barotropic vorticity equation are not solutions of the shallow-water equations (SWEs), Phillips' procedure was adopted by Williamson et al (1992) as a standard test case for shallow-water models and has been extensively used ever since (Jablonowski et al, 2009;Mohammadian and Marshall, 2010;Bosler et al, 2014;Ullrich, 2014;Li et al, 2015, are only five recent examples).…”
Section: Introductionmentioning
confidence: 99%
“…It has been introduced by [25] with a forward (explicit) and a backward (implicit) version, the latter being widely used in geosciences for global computations [94,64,80,86,84] and also in plasma dynamics [30,20,85,52]. Advection dominated problems, such as passive scalar transport, are good candidates for forward semi-Lagrangian approaches; e.g., methods have been recently proposed for weather or climate forecasts [22,14]. In the context of a disperse phase of droplets or particles, semi-Lagrangian methods are attractive because they are naturally compatible with the weakly-coupled nature of the material elements that are transported; i.e., weak diffusion and collisions, and slow or zero-velocity waves allow the characteristics to remain fairly independent of each other.…”
Section: Introductionmentioning
confidence: 99%
“…These N p trivial linear extrapolations exactly solve the transport part of the kinetic equation in the context of operator splitting. 2a) Gather (projection) according to the mapping of Eq (14)…”
mentioning
confidence: 99%
“…Instead he only examined qualitatively the spatial and temporal smoothness of his results and concluded that the emergent noise (manifested in the form of inertia-gravity (IG) waves) resulted from a small but significant divergence field that was missing from the initial conditions. Phillips' procedure was adopted by Williamson et al as part of their suite of test cases for numerical approximations of the SWEs and have been frequently used since (Jablonowski et al, 2009;Mohammadian and Marshall, 2010;Bosler et al, 2014;Ullrich, 2014;Li et al, 2015, are only five recent examples).…”
Section: Introductionmentioning
confidence: 99%