Published October 4, 2019
| Version v1
Publication
Multi-Scale Approximation of Thin-Layer Flows on Curved Topographies
Contributors
Others:
- National Cheng Kung University (NCKU)
- Societe Lemma [Biot]
- Control, Analysis and Simulations for TOkamak Research (CASTOR) ; Inria Sophia Antipolis - Méditerranée (CRISAM) ; Institut National de Recherche en Informatique et en Automatique (Inria)-Institut National de Recherche en Informatique et en Automatique (Inria)-Laboratoire Jean Alexandre Dieudonné (JAD) ; Université Nice Sophia Antipolis (1965 - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UCA)-Université Nice Sophia Antipolis (1965 - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UCA)
- COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)
- Laboratoire Jean Alexandre Dieudonné (JAD) ; Université Nice Sophia Antipolis (1965 - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UCA)
- Academia Sinica
Description
This paper is devoted to a multi-scale approach for describing the dynamic behaviors of thin-layer flows on complex topographies. Because the topographic surfaces are generally curved, we introduce an appropriate coordinate system for describing the flow behaviors in an e cient way. In the present study, the complex surfaces are supposed to be composed of a finite number of triangle elements. Due to the unequal orientation of the triangular elements, the distinct flux directions add to the complexity of solving the Riemann problems at the boundaries of the triangular elements. Hence, a vertex-centered cell system is introduced for computing the evolution of the physical quantities, where the cell boundaries lie within the triangles and the conventional Riemann solvers can be applied. Consequently, there are two mesh scales: the element scale for the local topographic mapping and the vertex-centered cell scale for the evolution of the physical quantities. The final scheme is completed by employing the HLL-approach for computing the numerical flux at the interfaces. Three numerical examples (the Ritter's solution, the Stoker's solution and the parabolic similarity solution) and one application to a large-scale landslide are conducted to examine the performance of the proposed approach as well as to illustrate its capability in describing the shallow flows on complex topographies.
Additional details
Identifiers
- URL
- https://hal.inria.fr/hal-02305269
- URN
- urn:oai:HAL:hal-02305269v1
Origin repository
- Origin repository
- UNICA