2011
DOI: 10.1016/j.jcp.2010.12.027
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Parallel multilevel methods for implicit solution of shallow water equations with nonsmooth topography on the cubed-sphere

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Cited by 30 publications
(23 citation statements)
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“…As a result, this test has been controversial in its usefulness [7,26]. Even so, it is still commonly used as a test case for novel numerical schemes in atmospheric modeling [7,30,35,48]. However, it should be noted that these instabilities necessitates the use of a filter, regardless of the numerical scheme.…”
Section: Rossby-haurwitz Wavesmentioning
confidence: 99%
“…As a result, this test has been controversial in its usefulness [7,26]. Even so, it is still commonly used as a test case for novel numerical schemes in atmospheric modeling [7,30,35,48]. However, it should be noted that these instabilities necessitates the use of a filter, regardless of the numerical scheme.…”
Section: Rossby-haurwitz Wavesmentioning
confidence: 99%
“…Although several studies have been carried out for these schemes for some linear problems, it is not clear which one is optimal for the Euler equations. In [48], κ = 0 is used for the global shallow water equations, while in [43], κ = 1/3 is used for the vertical discretization of the compressible Euler equations. In our finite volume scheme, we choose κ = 1/2 because of its low numerical dissipation as observed in our numerical experiments.…”
Section: Ausmmentioning
confidence: 99%
“…6.3]) and δX n is the Newton correction obtained by solving the Jacoian system as discussed later. To achieve a more uniform distribution of residual errors of all time steps [48], the stopping condition for the Newton iteration (5.1) is adaptively determined by…”
Section: Fully Implicit Adaptive Time Steppingmentioning
confidence: 99%
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