Prediction of time-evolving sand ripples in shelf seas
RL Soulsby, RJS Whitehouse, KV Marten - Continental Shelf Research, 2012 - Elsevier
The ability to predict the presence and physical properties of small-scale sand ripples on the
sea bed is important for determining the bed roughness felt by currents and waves, for …
sea bed is important for determining the bed roughness felt by currents and waves, for …
Probabilistic design and reliability analysis of scour protections for offshore windfarms
T Fazeres-Ferradosa, F Taveira-Pinto, X Romão… - Engineering Failure …, 2018 - Elsevier
Scour protection is an important component of fixed bottom foundations for offshore wind
turbines. Depending on the hydrodynamic conditions, they might be indispensable to avoid …
turbines. Depending on the hydrodynamic conditions, they might be indispensable to avoid …
The contribution of currents, sea‐swell waves, and infragravity waves to suspended‐sediment transport across a coral reef‐lagoon system
AWM Pomeroy, CD Storlazzi… - Journal of …, 2021 - Wiley Online Library
Coral reefs generate substantial volumes of carbonate sediment, which is redistributed
throughout the reef‐lagoon system. However, there is little understanding of the specific …
throughout the reef‐lagoon system. However, there is little understanding of the specific …
The influence of seasonal climate on the morphology of the mouth-bar in the Yangtze Estuary, China
M Zhang, I Townend, H Cai, J He, X Mei - Continental shelf research, 2018 - Elsevier
The geomorphology of the Yangtze Estuary in the Changjiang River Delta in Eastern China
has been the subject of extensive research. This study extends previous work to examine …
has been the subject of extensive research. This study extends previous work to examine …
[HTML][HTML] Seagrass meadows reduce wind-wave driven sediment resuspension in a sheltered environment
Seagrass meadows are prominent in many coastal zones worldwide and significant
contributors to global primary production. The large bottom roughness (or canopy) created …
contributors to global primary production. The large bottom roughness (or canopy) created …
Long-term evolution in the location, propagation, and magnitude of the tidal shear front off the Yellow River Mouth
N Wang, G Li, L Qiao, J Shi, P Dong, J Xu… - Continental Shelf Research, 2017 - Elsevier
Characteristics and formation of the tidal shear front off the Yellow River Mouth had been
previously studied based on observations and models. However, its long-term variability and …
previously studied based on observations and models. However, its long-term variability and …
[HTML][HTML] Bedform migration in a mixed sand and cohesive clay intertidal environment and implications for bed material transport predictions
Many coastal and estuarine environments are dominated by mixtures of non-cohesive sand
and cohesive mud. The migration rate of bedforms, such as ripples and dunes, in these …
and cohesive mud. The migration rate of bedforms, such as ripples and dunes, in these …
Current-and wave-generated bedforms on mixed sand–clay intertidal flats: A new bedform phase diagram and implications for bed roughness and preservation …
JH Baas, J Malarkey, ID Lichtman… - Frontiers in Earth …, 2021 - frontiersin.org
The effect of bedforms on frictional roughness felt by the overlying flow is crucial to the
regional modelling of estuaries and coastal seas. Bedforms are also a key marker of …
regional modelling of estuaries and coastal seas. Bedforms are also a key marker of …
Influence of cohesive clay on wave–current ripple dynamics captured in a 3D phase diagram
Wave–current ripples that develop on seabeds of mixed non-cohesive sand and cohesive
clay are commonplace in coastal and estuarine environments. While laboratory research on …
clay are commonplace in coastal and estuarine environments. While laboratory research on …
Impact of tidal shear fronts on terrigenous sediment transport in the Yellow River Mouth: Observations and a synthesis
N Wang, K Li, D Song, N Bi, X Bao, S Liang, G Li - Marine Geology, 2024 - Elsevier
A tidal shear front (TSF) can be defined as an obvious horizontal gradient of flow velocity
formed by opposing tidal currents (reversed TSF) or same-direction tidal currents …
formed by opposing tidal currents (reversed TSF) or same-direction tidal currents …