Characterizing bed roughness on the Antarctic continental margin
Spatial variability in bed topography, characterized as bed roughness, impacts ice-sheet flow and organization and can be used to infer subglacial conditions and processes, yet is difficult to quantify due to sparse observations. Paleo-subglacial beds of
Santiago Munevar Garcia +3 more
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Subglacial roughness of the Greenland Ice Sheet: relationship with contemporary ice velocity and geology [PDF]
The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly constrained both in its bulk properties, for example geology, the presence of sediment, and the presence of water, and interfacial conditions, such as roughness and bed rheology ...
M. A. Cooper +9 more
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Is the critical Shields stress for incipient sediment motion dependent on channel-bed slope? [PDF]
Data from laboratory flumes and natural streams show that the critical Shields stress for initial sediment motion increases with channel slope, which indicates that particles of the same size are more stable on steeper slopes.
Dietrich, William E. +2 more
core +1 more source
Quantifying bed roughness beneath contemporary and palaeo-ice streams
Bed roughness is an important control on ice-stream location and dynamics. The majority of previous bed roughness studies have been based on data derived from radio-echo sounding (RES) transects across Antarctica and Greenland.
FRANCESCA A.M. FALCINI +3 more
doaj +1 more source
Effect of near‐bed turbulence on chronic detachment of epilithic biofilm: Experimental and modeling approaches. [PDF]
The biomass dynamics of epilithic biofilm, a collective term for a complex microorganism community that grows on gravel bed rivers, was investigated by coupling experimental and numerical approaches focusing on epilithic biofilm‐flow interactions.
Ahmed Kettab +65 more
core +2 more sources
PREDICTING MOVABLE BED ROUGHNESS IN COASTAL WATERS [PDF]
Accurately predicting movable bed roughness is essential to the analyses of transport processes, but when the bottom is rippled, as it commonly is in the coastal environment, characterizing the roughness is less straightforward than when the bottom is flat.
Humbyrd, Chelsea Joy, Madsen, Ole S.
openaire +2 more sources
Formula of movable bed roughness for the Middle Yangtze River
The computation of movable bed roughness is an important step in morphodynamic models. After the operation of the Three Gorges Project (TGP), a dramatic decrease of sediment load entering the Middle Yangtze River (MYR) caused the processes of channel ...
Xin LIU +3 more
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Very-large-scale motions in rough-bed open-channel flow [PDF]
Acknowledgements The study has been supported by two EPSRC/UK grants, ‘High-resolution numerical and experimental studies of turbulence-induced sediment erosion and near-bed transport’ (EP/G056404/1) and ‘Bed friction in rough-bed free-surface flows: a ...
Cameron, S. M. +2 more
core +1 more source
The Influence of Bed Roughness on Turbulence: Cabras Lagoon, Sardinia, Italy
Estimates of bed roughness used for predictions of sediment transport are usually derived either from simple scalars of the physical roughness (i.e., ripple height or grain size) or from the hydrodynamic roughness length (Zo) based upon velocity gradient
Clémentine Chirol +5 more
doaj +1 more source
Bed-Load Effects on Hydrodynamics of Rough-Bed Open-Channel Flows [PDF]
The extent to which turbulent structure is affected by bed-load transport is investigated experimentally using a nonporous fixed planar bed comprising mixed-sized granular sediment with a d50 of 1.95 mm. Three different sizes of sediment ~d50= 0.77, 1.99, and 3.96 mm!
CAMPBELL L. J +5 more
openaire +3 more sources

