Reservoir Sedimentation 2014
DOI: 10.1201/b17397-8
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Meandering jets in shallow rectangular reservoir

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“…There are two groups of numerical models: depth‐resolving models [ Strauss and Glinsky , ; Yeh et al , ] and layer‐averaged models, which include the three‐equation model (TEM) and its variants [ Fukushima et al , ; Parker et al , ; Zeng and Lowe , ; Choi , ; Imran et al , ; Bradford and Katopodes , ; Kostic and Parker , , ; de Luna et al , ; Toniolo , ; Hu and Cao , ; Kostic et al , ; Eke et al , ; Hu et al , ; Lai and Wu , ; Kostic , ; Elfimov and Khakzad , ] and the Four‐Equation‐Model (FEM) and its variants [ Fukushima et al , ; Parker et al , ; Salaheldin et al , ; Pratson et al , ; Das et al , ; Fildani et al , ; Kostic and Parker , ; Yi and Imran , ; Eke et al , ; Kostic , ; Tracer et al , ]. The FEM differs from the TEM in the way in which the bed shear velocity ( u ∗ ) is computed [ Fukushima et al , ; Parker et al , ]: while the TEM computes u ∗ from the drag exerted on the bed, roughly approximated by TEM:1emu2=CDU2,where C D >0 is the bed drag coefficient and U the layer‐averaged velocity of the sediment‐water mixture, the FEM computes u ∗ from the assumption that the bed shear stress is proportional to the layer‐averaged turbulent kinetic energy ( k ), FEM:1emu2=αk,where α > 0 is the dimensionless proportionality constant.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…There are two groups of numerical models: depth‐resolving models [ Strauss and Glinsky , ; Yeh et al , ] and layer‐averaged models, which include the three‐equation model (TEM) and its variants [ Fukushima et al , ; Parker et al , ; Zeng and Lowe , ; Choi , ; Imran et al , ; Bradford and Katopodes , ; Kostic and Parker , , ; de Luna et al , ; Toniolo , ; Hu and Cao , ; Kostic et al , ; Eke et al , ; Hu et al , ; Lai and Wu , ; Kostic , ; Elfimov and Khakzad , ] and the Four‐Equation‐Model (FEM) and its variants [ Fukushima et al , ; Parker et al , ; Salaheldin et al , ; Pratson et al , ; Das et al , ; Fildani et al , ; Kostic and Parker , ; Yi and Imran , ; Eke et al , ; Kostic , ; Tracer et al , ]. The FEM differs from the TEM in the way in which the bed shear velocity ( u ∗ ) is computed [ Fukushima et al , ; Parker et al , ]: while the TEM computes u ∗ from the drag exerted on the bed, roughly approximated by TEM:1emu2=CDU2,where C D >0 is the bed drag coefficient and U the layer‐averaged velocity of the sediment‐water mixture, the FEM computes u ∗ from the assumption that the bed shear stress is proportional to the layer‐averaged turbulent kinetic energy ( k ), FEM:1emu2=αk,where α > 0 is the dimensionless proportionality constant.…”
Section: Introductionmentioning
confidence: 99%
“…There are two groups of numerical models: depth-resolving models [Strauss and Glinsky, 2012;Yeh et al, 2013] and layer-averaged models, which include the three-equation model (TEM) and its variants [Fukushima et al, 1985;Parker et al, 1986;Zeng and Lowe, 1997;Choi, 1998;Imran et al, 1998;Bradford and Katopodes, 1999;Parker, 2006, 2007;de Luna et al, 2009;Toniolo, 2009;Hu and Cao, 2009;Kostic et al, 2010;Eke et al, 2011;Hu et al, 2012;Lai and Wu, 2013;Kostic, 2014;Elfimov and Khakzad, 2014] and the Four-Equation-Model (FEM) and its variants [Fukushima et al, 1985;Parker et al, 1986;Salaheldin et al, 2000;Pratson et al, 2001;Das et al, 2004;Fildani et al, 2006;Kostic and Parker, 2006;Yi and Imran, 2006;Eke et al, 2011;Kostic, 2011;Tracer et al, 2012]. The FEM differs from the TEM in the way in which the bed shear velocity (u * ) is computed [Fukushima et al, 1985;Parker et al, 1986]: while the TEM computes u * from the drag exerted on the bed, roughly approximated by…”
Section: Introductionmentioning
confidence: 99%