WAVE-BY-WAVE PREDICTION in NARROWLY SPREAD SEAS USING FIXED-AND DRIFTING-POINT WAVE RECORDS: VALIDATION USING PHYSICAL MEASUREMENTS

Accurate and reliable phase-resolved prediction of ocean surface waves is crucial for many offshore operations in ocean engineering and marine science. One important application is in optimal control of a power take-off in a wave energy converter, leading to significantly higher power production. Our interest is the forecasting of wave fields based on measurements obtained from multiple upwave locations in moderate seas with small directional spreading angles, such as is prevalent along the south coast of Australia. The prediction model, based on FFTs and propagation of waves according to the linear dispersion relation, is applied to both wave groups and irregular wave fields generated in a wave basin and, additionally, to ocean waves measured with drifting wave buoys. To account for spreading, the model numerically advances linear, plane (i.e. long-crested) waves in space at an optimum offset angle equal to the underlying seastate root-mean-square spreading angle. Averaging predictions based on a few slightly separated measurement locations, each weighted according to the estimated variance of the individual prediction, is shown to be more accurate than that from any single location. We also assess in detail the effect of drifting-buoy measurements in both long-crested and short-crested seas using synthetic wave records and show that it is possible to satisfactorily reconstruct the signal at fixed points based on the Doppler shift felt by the drifting buoy. The reconstructed signals give much better predictions compared to those completely neglecting the effect of even rather slow drift.