“…Lewis and Olin [] and Coakley et al . [] succinctly suggest it is a Lambertian scatterer, for which case the incident angle dependency should follow a cosine law. In Figure , the cos θ (in dB, when compared against normal incidence) expected rate of decay of a Lambertian scatterer has been superimposed on the data.…”
Section: Discussionmentioning
confidence: 99%
“…To put the data in context, a summary of previous nearshore observations and the present data set are presented in Figure [ Kalmykov et al ., ; Lewis and Olin , ; Haller and Lyzenga , ; Farquharson et al ., ]. We have also included one laboratory data set by [ Coakley et al ., ], and data taken at 3° grazing by McLaughlin et al . [], although for very short waves, thus steepness limited, in a nearshore setting.…”
Section: Discussionmentioning
confidence: 99%
“…A second known characteristic of the scattering from breaking waves is that the mean Doppler spectrum is subject to broadening and bias to higher frequencies by sporadic, but large power, scattering events. The Doppler peak is shifted to high frequencies by scattering arising from the active breaking portion of the wave [e.g., Smith et al, 1996] with spectral broadening being driven by surface disturbances produced on the Journal of Geophysical Research: Oceans 10.1002/2014JC009880 turbulent front face that have a range of speeds about their spatial mean, which is the local wave celerity [e.g., Fuchs et al, 1999;Coakley et al, 2001;Farquharson et al, 2005]. All locations where breaking waves were identified, this shift and broadening were identified in the Doppler spectra.…”
Section: Discussionmentioning
confidence: 99%
“…To put the data in context, a summary of previous nearshore observations and the present data set are presented in Figure 18 Lewis and Olin, 1980;Haller and Lyzenga, 2003;Farquharson et al, 2005]. We have also included one laboratory data set by [Coakley et al, 2001], and data taken at 3 grazing by McLaughlin et al [1995], although for very short waves, thus steepness limited, in a nearshore setting. It is worth noting that these previously reported values correspond to peak NRCS, whereas our data has been presented in terms of median NRCS.…”
Section: 1002/2014jc009880mentioning
confidence: 99%
“…Despite the obviousness of the rough surface assumption, no specific model exists to predict the nature of the rough surface or the apparent independence from environmental parameters found here. Lewis and Olin [1980] and Coakley et al [2001] succinctly suggest it is a Lambertian scatterer, for which case the incident angle dependency should follow a cosine law. In Figure 18, the cos h (in dB, when compared against normal incidence) expected rate of decay of a Lambertian scatterer has been superimposed on the data.…”
The microwave backscatter properties of surf zone waves are analyzed using field observations. By utilizing a preexisting, independent, water surface discrimination technique, the microwave returns were extracted along individual waveforms and the data from shoaling (steepening) waves, surf zone breaking waves, and remnant foam were separated and quantified. In addition, a wave tracking analysis technique allows the returns to be examined on a wave-by-wave basis as individual waves progress through the shoaling zone and break on a nearshore sand bar. Normalized radar cross sections (NRCS), polarization ratios, Doppler spectra, and scatterer velocities were collected using a dual-polarized, X-band radar operating at lower grazing angles than previously reported (1 -3.5 ). The results indicate that the maximum NRCS levels are from the active breaking portions of the wave and were consistently about 220 dB, regardless of radar polarization, azimuth angle, wave height, or wind speed. In addition, breaking waves induce broadening of the Doppler spectra and mean scatterer velocities that correlate well with the carrier wave celerity. Analysis of the polarization ratios suggest that the active breaking portions of the wave are depolarized but that higher polarization ratios (>0 dB) are found on the leading edges shoreward of the active breaking portions of the waves, which indicates a clear distinction between two scattering regimes. These results are consistent with scattering from a very rough surface that is being mechanically generated by the breaking process, showing a good agreement with the expected grazing angle dependency of a Lambertian scatterer.
“…Lewis and Olin [] and Coakley et al . [] succinctly suggest it is a Lambertian scatterer, for which case the incident angle dependency should follow a cosine law. In Figure , the cos θ (in dB, when compared against normal incidence) expected rate of decay of a Lambertian scatterer has been superimposed on the data.…”
Section: Discussionmentioning
confidence: 99%
“…To put the data in context, a summary of previous nearshore observations and the present data set are presented in Figure [ Kalmykov et al ., ; Lewis and Olin , ; Haller and Lyzenga , ; Farquharson et al ., ]. We have also included one laboratory data set by [ Coakley et al ., ], and data taken at 3° grazing by McLaughlin et al . [], although for very short waves, thus steepness limited, in a nearshore setting.…”
Section: Discussionmentioning
confidence: 99%
“…A second known characteristic of the scattering from breaking waves is that the mean Doppler spectrum is subject to broadening and bias to higher frequencies by sporadic, but large power, scattering events. The Doppler peak is shifted to high frequencies by scattering arising from the active breaking portion of the wave [e.g., Smith et al, 1996] with spectral broadening being driven by surface disturbances produced on the Journal of Geophysical Research: Oceans 10.1002/2014JC009880 turbulent front face that have a range of speeds about their spatial mean, which is the local wave celerity [e.g., Fuchs et al, 1999;Coakley et al, 2001;Farquharson et al, 2005]. All locations where breaking waves were identified, this shift and broadening were identified in the Doppler spectra.…”
Section: Discussionmentioning
confidence: 99%
“…To put the data in context, a summary of previous nearshore observations and the present data set are presented in Figure 18 Lewis and Olin, 1980;Haller and Lyzenga, 2003;Farquharson et al, 2005]. We have also included one laboratory data set by [Coakley et al, 2001], and data taken at 3 grazing by McLaughlin et al [1995], although for very short waves, thus steepness limited, in a nearshore setting. It is worth noting that these previously reported values correspond to peak NRCS, whereas our data has been presented in terms of median NRCS.…”
Section: 1002/2014jc009880mentioning
confidence: 99%
“…Despite the obviousness of the rough surface assumption, no specific model exists to predict the nature of the rough surface or the apparent independence from environmental parameters found here. Lewis and Olin [1980] and Coakley et al [2001] succinctly suggest it is a Lambertian scatterer, for which case the incident angle dependency should follow a cosine law. In Figure 18, the cos h (in dB, when compared against normal incidence) expected rate of decay of a Lambertian scatterer has been superimposed on the data.…”
The microwave backscatter properties of surf zone waves are analyzed using field observations. By utilizing a preexisting, independent, water surface discrimination technique, the microwave returns were extracted along individual waveforms and the data from shoaling (steepening) waves, surf zone breaking waves, and remnant foam were separated and quantified. In addition, a wave tracking analysis technique allows the returns to be examined on a wave-by-wave basis as individual waves progress through the shoaling zone and break on a nearshore sand bar. Normalized radar cross sections (NRCS), polarization ratios, Doppler spectra, and scatterer velocities were collected using a dual-polarized, X-band radar operating at lower grazing angles than previously reported (1 -3.5 ). The results indicate that the maximum NRCS levels are from the active breaking portions of the wave and were consistently about 220 dB, regardless of radar polarization, azimuth angle, wave height, or wind speed. In addition, breaking waves induce broadening of the Doppler spectra and mean scatterer velocities that correlate well with the carrier wave celerity. Analysis of the polarization ratios suggest that the active breaking portions of the wave are depolarized but that higher polarization ratios (>0 dB) are found on the leading edges shoreward of the active breaking portions of the waves, which indicates a clear distinction between two scattering regimes. These results are consistent with scattering from a very rough surface that is being mechanically generated by the breaking process, showing a good agreement with the expected grazing angle dependency of a Lambertian scatterer.
A key feature of breaking bores, jumps and spilling breakers is the roller region, characterised by intense shear and recirculation, associated with air bubble entrainment and splashing. Detailed unsteady air-water flow measurements were conducted in a breaking bore propagating in a largesize channel, using an array of dual-tip phase detection probes and an ultra-high-speed video camera. The results showed a steep roller front, with a very-dynamic air-water bubbly region, albeit with a relatively limited air-water roller region. In this study, a major challenge was the inconsistency in light intensity linked to the travelling nature of the bore. A simple flow visualisation technique was applied to retrieve the two-dimensional side-looking profile of the roller edge and average void fraction. The results were validated independently with a phase-detection probe. While the probe data lacked spatial variability, the study reinforces the needs of high quality validation dataset, including in unsteady transient flows.
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