1986
DOI: 10.1002/fld.1650060605
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Finite element method for moving boundary problems in river flow

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Cited by 100 publications
(42 citation statements)
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“…The problem, which was proposed by Kawahara and Umetsu (1986) m with initial water depth  = 1.875 m, while the rest of the channel is considered dry. Three humps are located in the channel bottom.…”
Section: Dam-break Flooding Over Three Humpsmentioning
confidence: 99%
“…The problem, which was proposed by Kawahara and Umetsu (1986) m with initial water depth  = 1.875 m, while the rest of the channel is considered dry. Three humps are located in the channel bottom.…”
Section: Dam-break Flooding Over Three Humpsmentioning
confidence: 99%
“…이 외에도 자연하천에서의 마름/젖음 처리를 위해서 Benque et al (1982)은 ADI (Alternating Direction Implicit)를 이용한 유한차분법을 개발하였으나 이 기법 은 유속과 수위가 급격히 변하는 경우에는 부정확한 해를 도출하였다 (Kawahara and Umetsu, 1986). Samuels (1985)는 홍수터에서의 부정류 해석을 위해서 유한요소기법을 이용하였고, Katopodes (1987) …”
Section: 서 론unclassified
“…On peut en attendre une précision moyenne de 10 % sur les vitesses intégrées verticalement. Cette méthode est devenue au cours de la dernière décennie un outil reconnu scientifiquement pour la simulation des écoulements dans les rivières, les fleuves et les estuaires (voir entre autres HERRLING, 1982 ;KAWAHARA et UMETSU, 1986 ;LECLERC et ai, 1987, 1990b, c).…”
Section: Modèle Hydrodynamique Bidimensionnel De Saint-venantunclassified