Minutes of Hydralab's 3rd advanced workshop:
, 2018 As part of the fourth HYDRALAB Workshop Event, the third advanced JRA 1 RECIPE workshop was organized around the issues addressed within the task 8.3 - scaling morphodynamics in time...
Henry, Piere-Yves, Aberle, Jochen
openaire +2 more sources
Hydralab+ Deliverable D8.3 Protocols for scaling morphodynamics in time
, 2018 This deliverable reviews the current knowledge and know-how regarding the scaling of time-dependent morphodynamic processes in physical laboratory studies, to address the climate change related evolution of different kinds of aquatic environments ranging from fluvial to coastal systems. Based on this review, protocols are derived to aid with the design
Henry, Pierre-Yves, Aberle, Jochen
openaire +2 more sources
Wave patterns generated by an axisymmetric obstacle in a two-layer flow [PDF]
, 2013 Gravity waves generated by a moving obstacle in a two-layer stratified fluid are investigated. The experimental configuration is three-dimensional with an axisymmetric obstacle which is towed in one of the two layers.
A Benetazzo +34 more
core +5 more sources
An analysis of nearshore profile and bar development under large scale erosive and accretive waves [PDF]
, 2018 This is an Accepted Manuscript of an article published by Taylor & Francis Group in Journal of Hydraulic Research on 2018, available online at: http://www.tandfonline.com/10.1080/00221686.2017.1315748Typical morphodynamic laboratory tests have been ...
Cáceres Rabionet, Iván +1 more
core +2 more sources
Effect and propagation of water level fluctuations in a sloping sandy beach -- Unsaturated porous media II: numerical simulation test of single harmonic wave (long run) [PDF]
, 2012 In coastal processes, the strong water movements due to short periodic waves (such as sea swell) can induce irregular water level fluctuations in the swash zone and within the sandy beach.
Ababou, Rachid +2 more
core +2 more sources
Hydrodynamics and morphodynamics in the swash zone: hydralab III large-scale experiments [PDF]
, 2011 The modelling of swash zone hydrodynamics and sediment transport and the resulting morphodynamics has been an area of very active research over the last decade. However, many details are still to be understood, whose knowledge will be greatly advanced by the collection of high quality data under controlled large-scale laboratory conditions.
openaire +1 more source
Large scale experiments on beach evolution induced by bichromatic wave groups with varying group period [PDF]
, 2014 New large scale experimental data have been presented showing the wave group influence on beach morphodynamics at the surf and swash zones. Bichromatic wave conditions were generated varying the modulation bandwidth but keeping the wave energetic content
Alsina, Jose M. +4 more
core +3 more sources
Physical modelling of water, fauna and flora: knowledge gaps, avenues for future research and infrastructural needs [PDF]
, 2014 peer reviewedPhysical modelling is a key tool for generating understanding of the complex interactions between aquatic organisms and hydraulics, which is important for management of aquatic environments under environmental change and our ability to ...
Bouma, Tjeerd +22 more
core +1 more source
, 2019 The measurement of wave and / or ice loads on coastal and maritime structures can play an important role in their final design. The number and range of man-made structures that are subject to these loads is increasing – from offshore oil and gas facilities, through ships and, renewable energy devices, to breakwaters, quay walls, bridges and tunnels ...
Sutherland, James, Evers, Karl-Ulrich
openaire +2 more sources
Comparative analysis of suspended sand concentration recorded with different techniques in a rippled bed regime [PDF]
, 2010 Sediment entrainment processes due to the oscillatory flow above rippled and plane sea beds are fundamentally different. Whereas above plane beds the sheet flow or bed load regime dominates and the momentum transfer is primarily caused by turbulent ...
Ahmari, Alireza +2 more
core +2 more sources