Results 71 to 80 of about 8,018 (216)
Reynolds and froude number effect on the flow past an interface-piercing circular cylinder
International Journal of Naval Architecture and Ocean Engineering, 2014 The two-phase turbulent flow past an interface-piercing circular cylinder is studied using a high-fidelity orthogonal curvilinear grid solver with a Lagrangian dynamic subgrid-scale model for large-eddy simulation and a coupled level set and volume of ...
Koo Bonguk +3 more
doaj +3 more sources
From Lotic to Lentic: SWOT Characterizes Seasonal Hydrodynamics in the Lake‐River Continuum
Geophysical Research Letters, Volume 53, Issue 11, 16 June 2026.Abstract The interface between rivers and lakes forms a unique hydraulic continuum, in which lotic and lentic regimes dynamically interact and transition between each other. A common expression of this lake‐river continuum (LARIC) is reservoir backwater, where water surface gradually rises from the reservoir pool upstream to the free‐flowing river ...
Xinchen He +7 more
wiley +1 more source
Nonlinear high-froude-number free-surface problems [PDF]
Journal of Engineering Mathematics, 1967 Peer Reviewed ; http://deepblue.lib.umich.edu/bitstream/2027.42/42698/1/10665_2005_Article_BF01540946 ...
openaire +2 more sources
Convective Froude Number and Byram's Energy Criterion of Australian Experimental Grassland Fires [PDF]
, 2015 A subset of experimental fires, conducted in the Northern Territory, Australia, in July and August 1986, was analysed to examine the role of the convective Froude number and Byram's energy criterion (Pw/P f) in the behaviour of grassland fires.
Sullivan, Andrew
core +1 more source
Erosion of granular sediments by submerged impinging jets: Particle size effects and cohesion onset
AIChE Journal, Volume 72, Issue 6, June 2026.Abstract This study investigates the erosion behavior and modeling of glass particle beds under impinging jet conditions, with a focus on particle size effects and the onset of cohesion. Ultrasonic profiling is implemented to scan and measure static crater profiles.
Ahmad Mohamadiyeh +4 more
wiley +1 more source
The Depositional Record, Volume 12, Issue 3, June 2026.We document meter‐scale antidune and cyclic‐step deposits in channel–lobe transition zone (CLTZ) deposits of the Upper Cretaceous Point Loma Formation in San Diego, California. These results provide new insights into sediment transport dynamics in CLTZ environments, which are critical for understanding reservoir connectivity and heterogeneity in ...
Luthfi Saifudin +4 more
wiley +1 more source
International Journal of Mechanical System Dynamics, Volume 6, Issue 2, Page 247-266, June 2026.ABSTRACT This study investigates the hydrodynamic influence of forward transom tapering on a displacement catamaran hull using computational fluid dynamics (CFD) simulations. Five taper configurations ranging from a vertical transom base design to a fully tapered stern (1.00B) were evaluated over a wide Froude number range (Fr = .3 to 1.0).
Chalermkiat Nuchturee +3 more
wiley +1 more source
Journal of Marine Science and Engineering, 2020 Understanding the propagation of landslide-generated water waves is of great help against tsunami hazards. In order to investigate the effects of landslide shapes on the far-field leading wave generated by a submerged landslide at a constant depth, three
Haixiao Jing +3 more
doaj +1 more source
Numerical Modeling of Inertial Particles in Three‐Dimensional Fluid Flow
Proceedings in Applied Mathematics and Mechanics, Volume 26, Issue 2, June 2026.ABSTRACT The motion of inertial particles in a fluid is modeled by the Maxey–Riley–Gatignol equation (MaRGE). The MaRGE contains an integral term that arises due to the viscous diffusion of vorticity in the fluid around the particle. Because it makes MaRGE difficult to solve numerically, the integral term is often neglected or approximated, despite its
Vamika Rathi, Daniel Ruprecht
wiley +1 more source
Stratified separated flow around a mountain with an inversion layer below the mountain top
, 2006 This paper presents analytical and numerical results for separated stratified inviscid flow over and around an isolated mountain in the limit of small Fronde number.
Johnson, ER, Vilenski, GG, Hunt, JCR
core