The Profile Volume Approach to Beach Nourishment
The purpose of this paper is to outline a design approach to beach nourishment that emphasizes profile volumes. The advantages and disadvantages of the method are discussed and related...
Holding a Shorelind with a Buried Revetment
Two shoreline modification projects were designed that use a new application of an old idea to provide erosion protection and improve shoreline access and aesthetics. The innovation consists...
Forecasting Wave Attenuation Performance for Marinas
A methodology is presented for interpreting the performance of a dynamically acting floating attenuator in a field of irregular waves. The analysis explains the physical significance of...
Coastal Processes on the Wai-San-Ding Barrier of Taiwan STrait, R.O.C.
The coastal line processes on the Wan-San-Ding Barrier is discussed in this paper since 1900. The wave energy along this coast is computed from the measured wave by considering the refraction...
Wave-Induced Erosion on a Tidal Marsh Shoreline in Corte Madera Bay
One of the primary factors controlling the formation and configuration of a shoreline is the interaction of waves with the shore. A monitoring program was set up at the Corte Madera Ecological...
A Cooperative Coastal Data Collection Program in Washington State
The Washington State Department of Ecology and the U.S. Army Corps of Engineers have initiated a cooperative agreement for the joint management and funding of the Washington Coastal Data...
The Coastal Data Information Program?A Successful Federal, State and University Cooperation
The Coastal Data Information Program (CDIP) is a cooperative effort managed jointly by the U.S. Army Engineers, Waterways Experiment Station and the State of California, Department of...
Vertical Distribution of Sediment Under Waves
This paper is based on the research foundation of vertical relative distribution of sediment concentration and alluvial bed stability under waves. Amended theories of E. W. Lane and A.A....
Bank Erosion at the Aransas National Wildlife Refuge
The Aransas National Wildlife Refuge has been experiencing problems with the erosion along the banks of the Gulf Intracoastal Waterway. In order to prevent future erosion it is necessary...
Berm Placement Planning Study at Breton Island, Louisiana
This paper identifies tools that are being utilized to determine the most environmentally beneficial location for a nearshore berm to be constructed at Breton Island, Louisiana. The computer...
Transformation of the Black Sea Coast and Shelf by Wave Erosion in Pliocene-Pleistocene
Theory of transformation of coast and shelf of the ancient and modern seas by waves is presented. It allows to work out a scheme of adjoining land and shelf evolution on the basis of basin...
The Specific Peculiarities of Relief Transformation and Shelly Sediment Differentiation in Coastal Zone
The settling velocities values of shelly sediment considerably differ from ones of the same particles of terrigeneous material and for this reason character and intensity of hydrodynamic...
Wave Boundary Layer Above the Submerged Coastal Slope
A calculation method of parameters of turbulent boundary layer formed by waves is proposed. A calculation of boundary layer on a rough slope with inclination typical for steep Caucasian...
Ecological Situation of the Black Sea Coastal Zone
Some aspects of the Black Sea ecosystems evolution are discussed with regard of growing volumes of discharged pollutants and encroachment of Mnemopsisleidyi. The data characterizing ecological...
Scientific Basis of Regulation of Coastal Processes (Case Study: Coast of the Black Sea)
SIA Saknapirdatsva experience in creation of gravel beaches for the coast protection from wave erosion is generalized in this paper. A conclusion has been made that the most expedient...
Development and Modern Dynamics of Alluvial-Accumulative Coasts of the Eastern Black Sea
River regime, river sediment and wave processes are greatly important in the alluvial accumulative coast evolution. The Black Sea coast of the Georgia may be a good example of such coast...
Regularities of the Abrasive Coast Development of the Ukrainian Black Sea
The length of the Ukrainian Black Sea coast between Danube delta and Kerch Strait is 1628 km. Abrasive cliffs with rates of abrasion from 0.1 to 4.7 m/y (average multi-year data) are common....
South Coast of the Crimea: Environmental Specificity and Coast Protection Problems
Climate conditions and geological structure of the Crimean South coast are described in this paper. Morphometrical data on submerged coast slope are given. Today, out of 100 km of the...
Waves and Currents Near the Kinburn Spit Extremity
A method of calculation of wave transformation and of currents generated by waves in a surf zone, including a spit extremity is offered. No additional hypothesis on radial stress and wave...
The Flows of Suspended Sandy Material Along the Section of Bulgarian Coast
Combining of available models of elementary hydro- and lithodynamic processes in a single calculation scheme permits to evaluate the volumes of detrital material transported either way...
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