A time-centered split for implicit discretization of unsteady advection problems
Environmental flows (e.g. river and atmospheric flows) governed by the shallow water equations (SWE) are usually dominated by the advective mechanism over multiple time-scales. The combination of time dependency and nonlinear advection creates difficulties in the numerical solution of the SWE. A ful...
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| Format: | Others |
| Language: | English |
| Published: |
2008
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| Online Access: | http://hdl.handle.net/2152/3844 |