How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra? William J....
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![Page 1: How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra? William J. Plant, APL/UW, SoMaR, July 14, 2015.](https://reader036.fdocuments.us/reader036/viewer/2022062407/56649f4e5503460f94c6ef56/html5/thumbnails/1.jpg)
How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra?
William J. Plant, APL/UW, SoMaR, July 14, 2015
![Page 2: How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra? William J. Plant, APL/UW, SoMaR, July 14, 2015.](https://reader036.fdocuments.us/reader036/viewer/2022062407/56649f4e5503460f94c6ef56/html5/thumbnails/2.jpg)
![Page 3: How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra? William J. Plant, APL/UW, SoMaR, July 14, 2015.](https://reader036.fdocuments.us/reader036/viewer/2022062407/56649f4e5503460f94c6ef56/html5/thumbnails/3.jpg)
VV = Solid HH = Dashed
X-Band7 m/s
Plant, JGR, 1997
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Range, m
Tim
e, s
ec
fro
m s
tart
Detrended o (dB): Antenna 2
200 400 600 800 1000 1200
50
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-10
-5
0
5
10
Range, m
Tim
e, s
ec
fro
m s
tart
Det Vel (NaN at low SNR) (m/s): Antenna 2
200 400 600 800 1000 1200
50
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-2
-1
0
1
2
Range, m
Tim
e, s
ec
fro
m s
tart
Velocity Spread (m/s): Antenna 2
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0
1
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Wavenumber, rad/m
Fre
qu
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cy
, Hz
o Spectrum: Antenna 2
-0.4 -0.2 0 0.2 0.4-0.5
0
0.5
0.01
0.02
0.03
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0.05
Wavenumber, rad/m
Fre
qu
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cy
, Hz
Velocity Spectrum: Antenna 2
File No. 1660
Ant Look to 333 degT
Wind Vel 7.5 m/s from 333 degT
Ship Vel 0.5 m/s to 346 degT
Current 0.45 m/s from 346 degT
Vel Sprd Threshold 0 m/s-0.4 -0.2 0 0.2 0.4-0.5
0
0.5
0.01
0.02
0.03
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0.05
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Distance East, m
Dis
tanc
e N
orth
, m
Surface Displacement in m at t = 0 (White is cut along x = 82 m.)
0 50 100 150 200 2500
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-2
-1
0
1
2
Distance North, m
Tim
e, s
ec
Space/Time Image of Velocity in m/s Along Northerly Cut
0 50 100 150 200 2500
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-2
-1
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Wavenumber, rad/m
Fre
quen
cy,
Hz
Spectrum of Velocities in the Space/Time Image (dBm3s-1)
Ks_rng = -1 to 2 (Unidirectional)
kw_rng = 1 to 16; phi_rng = 1 to 31
fetch = 500 km; Wind Speed = 7.5 m/s
Inc = 80 deg, Breaking slope = 13 deg, <Vbr> = 2 m/s
<Min Slope> = -19.375 Deg
Wind waves: A = 0.33 m, = 63 m from 360
Swell: A = 0 m, = 95 m from -90 deg
Speed of dominant wind wave = 9.9 m/s
Speed of modulation pattern in x/t image = 3.6 m/s
Speed from linear spectral feature = 3.2 m/s-0.4 -0.2 0 0.2 0.4
-0.5
0
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-60
-40
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Data SimulationWith Breaking
Distance East, m
Dis
tanc
e N
orth
, m
Surface Displacement in m at t = 0 (White is cut along x = 82 m.)
0 50 100 150 200 2500
50
100
150
200
250
-2
-1
0
1
2
Distance North, m
Tim
e, s
ec
Space/Time Image of Velocity in m/s Along Northerly Cut
0 50 100 150 200 2500
20
40
60
80
100
120
-2
-1
0
1
2
Wavenumber, rad/m
Fre
quen
cy,
Hz
Spectrum of Velocities in the Space/Time Image (dBm3s-1)
Ks_rng = -1 to 2 (Unidirectional)
kw_rng = 1 to 16; phi_rng = 1 to 31
fetch = 500 km; Wind Speed = 7.5 m/s
Inc = 80 deg, Breaking slope = 45 deg, <Vbr> = 2 m/s
<Min Slope> = -19.2824 Deg
Wind waves: A = 0.33 m, = 63 m from 360
Swell: A = 0 m, = 95 m from -90 deg
Speed of dominant wind wave = 9.9 m/s
Speed of modulation pattern in x/t image = 4.3 m/s
Speed from linear spectral feature = -4.5 m/s-0.4 -0.2 0 0.2 0.4
-0.5
0
0.5
-60
-40
-20
0
20
SimulationWithout Breaking
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Plant, GRL, 2012
o o
o Ding and Farmer Acoustic Tracking
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So far I believe the material presented to be pretty well established.
Now I begin to speculate
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From Trokhimovski, JTech, 2000
Trokhimovski, Radiometer
Hwang et al., Tank, 1993
Hwang et al., Field, 1996
Friction Velocity about 25 cm/s
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Speculation:
This peak in B is caused by the breakers moving at the speed of the downwind interference pattern.
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Plant, JGR, 2015
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Combine f-k Spectra with Speeds of Breakers4 m/s 2 m/s 4 m/s 2 m/s
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8 40 200 800
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From Hwang and Wang, GRL, 2004
Dissipation Rate:“In the middle range (about 3<k<40 rad/m or0.16<λ<2.1 m), the dependence [of dissipation on wavenumber] is as strong as B10, approaching a delta function.”
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Contour plots of constant spectral density from Banner et al. (JFM, 1989), their figures 6 and 7. Left: Wind speed 5.5 m/s from the right (East). Right: Wind speed 13.3 m/s from the left (West) . The short lines in the fourth quadrant give the confidence intervals
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From Yueh et al., TGRS, 2013 L-Band, Inc = 29-46 degkb ≈ 41 rad/m
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0.6 rad/m to 40 rad/m 100 rad/m to 800 rad/m
Speeds match those of downwind interference pattern if advection by orbital velocities in
taken into account.
Peak of X-band Low-Grazing-Angle HH Doppler spectra match those of downwind
interference pattern
Greatly increased dissipation rates according to Hwang and Wang (2004).
Curvature spectrum peaks in this range.
Group speeds match those in the higher range
Group speeds match those in the lower range.
At low wind speeds, crosswind spectra are larger than downwind ones
Upwind spectra always larger than downwind ones.
Much wave breaking Unexplained Roughness
SPECTRAL FEATURES, MANY UNUSUAL
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8 40 200 800
L XC
1450
Ka
Ku K( Bragg Wavenumber at 10o Grazing )
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VV = Solid HH = Dashed
X-Band7 m/s
Plant, JGR, 1997
![Page 19: How Do Breaking Waves Show Up In Low-Grazing Angle Backscatter and Ocean Wave Spectra? William J. Plant, APL/UW, SoMaR, July 14, 2015.](https://reader036.fdocuments.us/reader036/viewer/2022062407/56649f4e5503460f94c6ef56/html5/thumbnails/19.jpg)
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Plant, GRL, 2012, Figure 4b