Results 61 to 70 of about 638 (182)
EVALUATION OF MEAN WAVE OVERTOPPING AND MAXIMUM INDIVIDUAL WAVE OVERTOPPING ON ROCK REVETMENT
Jurnal Teknologi (Sciences & Engineering)An accurate estimation of wave overtopping discharge on rock revetment is important to protect coastal areas from possible hazards. The mean discharge value is often used in the coastal structural design. However, the anticipated impact of the maximum volume of overtopping by individual waves is expected to be significant in wave overtopping ...
Mohd Shahrizal Ab Razak +4 more
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Maturation of River‐Dominated Delta Tops: The Channelized Delta Model
Water Resources Research, Volume 62, Issue 7, July 2026.Abstract We present a novel, laterally averaged model of delta growth, the channelized delta model, in which delta top dynamics are described in terms of channelized (lumped channel) and non‐channelized areas. The maturation level of the lumped channel is defined by a shape factor that dictates flow partitioning between channelized and non‐channelized ...
M. J. Czapiga, E. Viparelli, G. Parker
wiley +1 more source
Coastal Engineering 2006, 2007 This paper presents an expression describing the vertical distribution of overtopping, the experimental work leading to this, as well as the use of the expression for numerical optimization of the geometrical layout of the multi level overtopping based wave energy converter Seawave Slot-cone Generator.
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HYDRODYNAMIC LOAD ON THE BUILDING CAUSED BY OVERTOPPING WAVES [PDF]
Coastal Engineering Proceedings, 2012 Wide crested dike can reduce the kinetic energy of the overtopping wave and make the overtopping wave to flow back to the seaside. If a coastal town were built on or near a dike, the overtopping wave running on the dike crest generates the force which can affect the buildings located in its path.
Chen, X. (author) +6 more
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Paleoceanography and Paleoclimatology, Volume 41, Issue 7, July 2026.Abstract Sedimentary archives of tropical cyclones have been primarily developed in back barrier settings and karst basins at low to mid‐latitude sites in the Atlantic. Here, a unique record of high‐latitude storms is presented from Skan Bay, Unalaska in the Eastern Aleutian Islands. Storm‐induced coarse deposits in a 20.5 m composite sediment core are
Kelly McKeon +17 more
wiley +1 more source
Journal of Marine Science and EngineeringThis research examines the overtopping volumes associated with focused wave groups on smooth dikes with an emerged toe. Focused wave groups are employed to represent the highest waves of random sea states in a compact form, obviating the need to model ...
Corrado Altomare, Xavi Gironella
doaj +1 more source
COMPARISON OF NUMERICAL AND EXPERIMENTAL RESULTS FOR OVERTOPPING DISCHARGE OF THE OBREC WAVE ENERGY CONVERTER [PDF]
Journal of Engineering Science and Technology, 2017 OBREC is the latest innovation of overtopping wave energy converter (WEC) which is coalesced with the rubble mound breakwaters. The acquisition of wave overtopping in a front reservoir and consequently releasing process through turbine is the concept of ...
A. YAZID MALIKI +4 more
doaj
Water Resources Research, Volume 62, Issue 7, July 2026.Abstract The presence of a reservoir along a river modifies downstream flood events by storing and releasing water volumes. By attenuating the peak flows, the structure significantly alters their corresponding probability distributions, particularly in terms of the shape of the distribution.
S. Cipollini +3 more
wiley +1 more source
Numerical Investigation of Storm Surge Effects on Denitrification in Nearshore Aquifers
Water Resources Research, Volume 62, Issue 7, July 2026.Abstract Coastal aquifers are highly dynamic environments, sensitive to both regular hydrodynamic forcing and extreme events. Among these, storm surges can significantly alter subsurface flow by expanding the upper saline plume (USP), modifying residence times, and intensifying mixing between fresh groundwater and seawater.
Wenjin Song +3 more
wiley +1 more source
Boreas, Volume 55, Issue 3, Page 717-750, July 2026.Map of Lower sediment (LS) thickness is a surrogate for the distribution of Thorncliffe Formation (TF) and ~75% of TF thickness from the slope of Niagara Escarpment east to Brighton. Inset images show the LS sequence at the Don Valleys brickyards (DVBY) and undeformed TF sand and gravel (~15 m) below Newmarket Till (NT) at sites L and Co.
David R. Sharpe +3 more
wiley +1 more source