2010
DOI: 10.1016/j.cpc.2010.02.019
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A kinetic flux-vector splitting method for the shallow water magnetohydrodynamics

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Cited by 13 publications
(6 citation statements)
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“…This problem has been also considered in [4,10,16,23]. In this problem, the variable bottom topography is given as The initial data are and the value of gravitational acceleration is g = 1.…”
Section: Problem 2 Strong Riemann Problemmentioning
confidence: 99%
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“…This problem has been also considered in [4,10,16,23]. In this problem, the variable bottom topography is given as The initial data are and the value of gravitational acceleration is g = 1.…”
Section: Problem 2 Strong Riemann Problemmentioning
confidence: 99%
“…This problem is taken from [4,10,16]. The initial data are Here, the division of computational domain and value of g is the same as we considered in Problem 2.…”
Section: Problem 3 Weak Riemann Problemmentioning
confidence: 99%
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“…In the literature, there are some theoretical and numerical works available for studying the shallow water magnetohydrodynamic equations (for theoretical works, see [12][13][14]; for numerical works, see [15][16][17][18][19][20]). However, as far as we know, there has been very few work on the subject of the well-posedness of the shallow water magnetohydrodynamic equations addressed in the literature.…”
Section: Introductionmentioning
confidence: 99%