Supplementary Materials: Comparative Analyses between the Zero-Inertia and Fully Dynamic Models of the Shallow Water Equations for Unsteady Overland Flow Propagation
نویسنده
چکیده
The two numerical models applied in this paper are based on a time-splitting approach, where a prediction and a correction problem are sequentially solved. For both the numerical procedures, it has been shown that the prediction and the correction steps have the characteristics of a convective and a diffusive problem, respectively [2–5]. For these reasons, we call the prediction system "convective prediction" (CP) system and the correction system "diffusive correction" (DC) system. Let's assume a general system of balance laws,
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Comparative Analyses between the Zero-Inertia and Fully Dynamic Models of the Shallow Water Equations for Unsteady Overland Flow Propagation
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