2021
DOI: 10.1029/2020jc016676
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On the Problem of Modeling the Boat Wake Climate: The Florida Intracoastal Waterway

Abstract: The boat traffic associated with the accelerating urbanization of coastal areas has a significant impact on the health of coastal ecosystems. In otherwise typically quiescent intracoastal and estuarine waterways, the transient wave activity created by boat traffic generates intermittent bursts of higher flow velocities, accelerations, and stresses on the bed, vegetation, and both bivalve and coral reefs. Although boat wakes may have relatively small heights in deep water, they grow, steepen, and break as they … Show more

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Cited by 16 publications
(10 citation statements)
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“…According to the method of stationary phase, these end-point contributions are formally smaller than those associated with the stationary points (where partial derivatives of g 1,2 vanish), however in certain instances (for example, when the dimensionless measure of acceleration is large) they help explain unexpected features in the timefrequency domain. For these end-point contributions, we say they occur at t = τ e , so that at the start and final times, we have τ = τ e = 0 and τ = τ e = t f , respectively; in both cases, the relevant k is given implicitly through (12) and the frequency is then computed via by the dispersion function (2). These contributions therefore correspond to frequencies ω as a function of time that can be plotted on top of the spectrograms.…”
Section: B Methods Of Stationary Phasementioning
confidence: 99%
See 2 more Smart Citations
“…According to the method of stationary phase, these end-point contributions are formally smaller than those associated with the stationary points (where partial derivatives of g 1,2 vanish), however in certain instances (for example, when the dimensionless measure of acceleration is large) they help explain unexpected features in the timefrequency domain. For these end-point contributions, we say they occur at t = τ e , so that at the start and final times, we have τ = τ e = 0 and τ = τ e = t f , respectively; in both cases, the relevant k is given implicitly through (12) and the frequency is then computed via by the dispersion function (2). These contributions therefore correspond to frequencies ω as a function of time that can be plotted on top of the spectrograms.…”
Section: B Methods Of Stationary Phasementioning
confidence: 99%
“…where the time coordinate is equivalent to (12). In order to derive the classical dispersion curve, we rewrite (13) as…”
Section: Geometric Argumentsmentioning
confidence: 99%
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“…This model contains a ship wake module added to the existing Boussinesq formulation, modelling vessels as a moving pressure source (Shi et al, 2018). The model was validated (Shi et al, 2018) using laboratory data (Gourlay, 2001) examining supercritical wake in various flow regimes including slow-moving, large container ships (Forlini et al, 2021). The model was first used to inform installation design by simulating conditions with and without the THGs, comparing maximum velocities and water surface elevations (Williams, Forthcoming 2022).…”
Section: Funwave-tvdmentioning
confidence: 99%
“…The tool we employ to achieve this goal is the spectrogram, which uses short-time Fourier transforms to decompose each wave signal from the fixed sensor into a time-frequency heat-map. In recent times, some success has been achieved in using spectrograms to identify different features of ship wakes (e.g., their transverse and divergent waves) observed in real shipping channels and in experimental towing tanks [2,3,[5][6][7][8][9][10][11][12][13]. The theory for this line of enquiry has been almost entirely for steadily moving ships [1,3,5,8], with very brief studies of accelerating ships moving in one direction [1,5].…”
Section: Introductionmentioning
confidence: 99%