Titlebook: Wave Kinematics and Environmental Forces; Papers presented at Society for Underwater Technology (SUT) Book 1993 Springer Science+Business

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Non-Linear Wave Current Interactionsticular, the presence of a strongly sheared current at the water surface is shown to produce a significant increase in both the crest elevation and the wave induced velocity field. These changes cannot be predicted by a simple Doppler shifted solution based on an “equivalent” uniform current.

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Non-Linear Wave Current Interactionsticular, the presence of a strongly sheared current at the water surface is shown to produce a significant increase in both the crest elevation and the wave induced velocity field. These changes cannot be predicted by a simple Doppler shifted solution based on an “equivalent” uniform current.

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Technical Update and Field Data from the New Generation Microwave Directional Wave Radartional, Shell UK Exploration and Production, and the UK Department of Energy. The study involved contributions from three scientists working in the fields of wave measurements (M J Tucker), statistics (R G Tickell) and kinematics (J R Chaplin). The findings and recommendations of this study have now

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Wave Kinematics — Measurement, Modelling and Applicationrated that directional wave spectra and wave kinematics may be routinely monitored..This presentation briefly addresses the measurement system, discusses various analysis techniques which have been applied to the data, and illustrate subsequent application of the information in numerical wave modell

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Non-Linear Wave Current Interactionsd by Dalrymple (1974), has been extended to incorporate a five layered description of the flow field. This model allows an accurate representation of a strongly sheared current, and at the same time minimises the discontinuity in the vorticity profile. A variety of wave-current combinations are inve

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