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1
Lecture I
The Sonar Equation
and
Signal Detection
Dr. Nicholas C. Nicholas
Applied Technology Institute
349 Berkshire Drive
Riva, Maryland 21140
888-501-2100/410-956-8805
Website: www.ATIcourses.com
Email: ATI@ATIcourses.com
ATI Course Schedule: http://www.ATIcourses.com/schedule.htm
ATI’s IP Networking Over Satellite: http://www.aticourses.com/sonar_principles_asw_analysis.htm
10 – Vol. 95 Register online at www.ATIcourses.com or call ATI at 888.501.2100 or 410.956.8805
Sonar Principles & ASW Analysis
Off The Course Tuition."
Summary
This course provides an excellent introduction to underwater sound and highlights how sonar principles are
employed in ASW analyses. The course provides a solid understanding of the sonar equation and discusses in-
depth propagation loss, target strength, reverberation, arrays, array gain, and detection of signals.
Physical insight and typical results are provided to help understand each term of the sonar equation. The
instructors then show how the sonar equation can be used to perform ASW analysis and predict the performance of
passive and active sonar systems. The course also reviews the rationale behind current weapons and sensor
systems and discusses directions for research in response to the quieting of submarine signatures.
The course is valuable to engineers and scientists who are entering the field or as a review for employees who
want a system level overview. The lectures provide the knowledge and perspective needed to understand recent
developments in underwater acoustics and in ASW. A comprehensive set of notes and the textbook Principles of
Underwater Sound will be provided to all attendees.
Instructors
Dr. Nicholas Nicholas received a B. S. degree from
Carnegie-Mellon University, an M. S.
degree from Drexel University, and a
PhD degree in physics from the Catholic
University of America. His dissertation
was on the propagation of sound in the
deep ocean. He has been teaching
underwater acoustics courses since
1977 and has been visiting lecturer at the U.S. Naval
War College and several universities. Dr. Nicholas has
more than 25 years experience in underwater acoustics
and submarine related work. He is working for Penn
State’s Applied Research Laboratory (ARL).
Dr. Robert Jennette received a PhD degree in
Physics from New York University in
1971. He has worked in sonar system
design with particular emphasis on long-
range passive systems, especially their
interaction with ambient noise. He held
the NAVSEA Chair in Underwater
Acoustics at the US Naval Academy
where he initiated a radiated noise measurement
program. Currently Dr. Jennette is a consultant
specializing in radiated noise and the use of acoustic
monitoring.
Course Outline
1. Sonar Equation & Signal Detection. Sonar
concepts and units. The sonar equation. Typical active
and passive sonar parameters. Signal detection,
probability of detection/false alarm. ROC curves and
detection threshold.
2. Propagation of Sound in the Sea.
Oceanographic basis of propagation, convergence
zones, surface ducts, sound channels, surface and
bottom losses.
3. Target Strength and Reverberation. Scattering
phenomena and submarine strength. Bottom, surface,
and volume reverberation mechanisms. Methods for
modeling reverberations.
4. Elements of ASW Analysis. Fundamentals of
ASW analysis. Sonar principles and ASW analysis,
illustrative sonobuoy barrier model. The use of
operations research to improve ASW.
5. Arrays and Beamforming. Directivity and array
gain; sidelobe control, array patterns and beamforming
for passive bottom, hull mounted, and sonobuoy
sensors; calculation of array gain in directional noise.
6. Passive Sonar. Illustrations of passive sonars
including sonobuoys, towed array systems, and
submarine sonar. Considerations for passive sonar
systems, including radiated source level, sources of
background noise, and self noise.
7. Active Sonar. Design factors for active sonar
systems including transducer, waveform selection, and
optimum frequency; examples include ASW sonar,
sidescan sonar, and torpedo sonar.
8. Theory and Applications of Current Weapons
and Sensor Systems. An unclassified exposition of the
rationale behind the design of current Navy acoustic
systems. How the choice of particular parameter values
in the sonar equation produces sensor designs
optimized to particular military requirements. Generic
sonars examined vary from short-range active mine
hunting sonars to long-range passive systems.
What You Will Learn
• Sonar parameters and their utility in ASW Analysis.
• Sonar equation as it applies to active and passive
systems.
• Fundamentals of array configurations, beamforming,
and signal detectability.
• Rationale behind the design of passive and active
sonar systems.
• Theory and applications of current weapons and
sensors, plus future directions.
• The implications and counters to the quieting of the
target’s signature.
SEE CURRENT SCHEDULE
FOR THE LATEST DATES
http://www.ATIcourses.com/schedule.htm
www.ATIcourses.com
Boost Your Skills
with On-Site Courses
Tailored to Your Needs
The Applied Technology Institute specializes in training programs for technical professionals. Our courses keep you
current in the state-of-the-art technology that is essential to keep your company on the cutting edge in today’s highly
competitive marketplace. Since 1984, ATI has earned the trust of training departments nationwide, and has presented
on-site training at the major Navy, Air Force and NASA centers, and for a large number of contractors. Our training
increases effectiveness and productivity. Learn from the proven best.
For a Free On-Site Quote Visit Us At: http://www.ATIcourses.com/free_onsite_quote.asp
For Our Current Public Course Schedule Go To: http://www.ATIcourses.com/schedule.htm
349 Berkshire Drive
Riva, Maryland 21140
Telephone 1-888-501-2100 / (410) 965-8805
Fax (410) 956-5785
Email: ATI@ATIcourses.com
2
What is Sound?
Sound is a mechanical wave motion propagating in an elastic
medium. Associated with this wave motion are changes in the
local pressure and density.
Sonar, an acronym for SOund NAvigation and Ranging, uses
sound energy (generally underwater) to transmit information.
3
Longitudinal Waves
COMPRESSIONS AND RAREFACTIONS OF LONGITUDINAL WAVES
λ = WAVELENGTH
f = FREQUENCY
c = SPEED OF SOUND
4
Terminology
Psycho/Physiological Physical
Pitch Frequency
(Nominal) Audible Range: 20 –20,000 Hz
Speech Range : 100 – 4,000 Hz
Infrasonic : Below audible range
Ultrasonic : Above audible range
Loudness Intensity
Intensity = 10 LOG10 I1/I0 = 20 LOG10 P1/P0 Decibels (dB)
Quality Waveform
Spectrum, Relative
amplitudes/phases
5
Nominal Speed of Sound
Material Speed of Sound (m/s) Density (g/cm3)
Aluminum (rolled) 6420 2.7
Stainless Steel 5790 7.9
Rubber, Gum 1550 0.95
Fresh Water (25oC) 1498 0.998
Sea Water (25oC) 1531 1.025
Air 331 0.0012
Sea Water 1430→1530
6
Acoustic Wavelength versus Frequency
Wavelength = sound speed/ frequency
λ = c/f
7
Sensitivity of the Human Ear
0 dB = 0.0002 dyne/ sq. cm
Shortly & Williams (53)
8
Doppler Shift (Passive Sonar)
When a sound source is moving with respect to an acoustic observer, the frequency
of the sound is shifted.
f0 = fs c + V0
c - Vs
f0 = observed frequency
fs = frequency at the source
c = speed of sound
V0 = speed of observer approaching sound source = V1 cos Θ
Vs = speed of source approaching observer = V2 cos Θ
Θ = bearing angle
Doppler shift is about 0.35 Hz per knot, about 1% at 30 knots
9
Doppler Shift (Active Sonar)
In active sonar, the approaching target received a signal which is shifted higher in
frequency (up-Doppler), then reradiates as a moving source approaching the
receiver, causing a doubling of the Doppler shift.
f = 0.69 Hz/(knot) (KHz) [ACTIVE]
REMEMBER
Approaching target produces an up-Doppler.
Receding target produced a down-Doppler.
Active sonar Doppler shift is double that of passive sonar
(about 2% at 30 knots)
10
Lofargram of Simulated Aircraft Overflight
11
Decibel (dB)
Decibels are 10 times the logarithm (to base 10) of
the ration of a power or power-related quantity
divided by a reference level.
I (dB re 1 watt/cm2) = 10 log I (watts/cm2)
Iref
(watt/cm2)
Remember the following properties of logarithms:
log 10X = X
log [10X 10Y] = log 10(X+Y) = X+Y
To convert from dB to linear units
i (linear ratio) = 10(0.1)I
Where i = linear ration normalized by reference unit
I = dB value.
12
Intensity/Pressure/Acoustic Impedance
Intensity is the (sound) power flow per unit area
I = P2 / ρc
where P = pressure amplitude
ρc = acoustic impedance
ρ = density
c = speed of sound
Intensity = 10 log I/Iref
= 10 log (P/Pref )2
= 20 log P/P2
13
Pressure Units
- Force per unit area
- MKS units:
1 Pascal = 1 Newton/m2
- CGS units:
1 µbar = 1 dyne/cm2
-New reference unit
1 µPascal = 10-6 Newton/m2
14
Power Addition
It is sometimes necessary to sum powers of two numbers which are expressed
by dB. The numbers cannot be simply summed in dB form, as that would
correspond to multiplication. In order to sum power, first convert from dB to
the original units, add, and then express the result in dB. Alternately, the
following curve can be used.
15
EXAMPLE FOR THE COMBINATION OF
SHIPPING NOISE AND WIND WAVE NOISE
EXAMPLE FOR DETECTION THRESHOLD = -5 dB
(S/N)REQ = -5 dB
[(S+N/N)]REQ = 1.2 dB
16
More Examples
If the acoustic pressure in a plane wave is increased by a
factor of 3, what is the change in level of the sound?
If the acoustic intensity in a plane wave is increased by a
factor of 3, what is the change in level of the sound?
If the acoustic pressure in a plane wave is reduced to 1/4,
what is the change in level of the sound?
If the acoustic intensity in a plane wave is reduced to
1/10, what is the change in level of the sound?
17
Yet More Examples
At a certain location the noise level due to oceanic
turbulence is 70 dB, the noise level due to distant
shipping is 73 dB, and the self-noise level is 73 dB.
What is the total noise level?
18
Bathymetry
Illustration of bathymetrically unimpeded ray paths emanating from Herd Islands with the
indicated launch angles. All rays are refracted geodesics along the surface containing the sound
channel axis. White boxes indicate locations of oceanographic research stations capable of receiving
acoustic signals. (Munk and Forbes, 1989; J. Phys. Oceanography, No. 19, 1965-78; copyright by
the American Meteorological Society)
19
Generalized Shipping Routes
20
Noise Spectra
21
Bathymetry and Sound Speed Structure
22
Ambient Noise Measurements
Paul C. Etter, Underwater Acoustic
Modeling, E & F SPON,
New York, NY, Second Edition, 1996
23
Bathymetric and Sound Speed Structure
(North Pacific)
Paul C. Etter, Underwater Acoustic
Modeling, E & F SPON,
New York, NY, Second Edition, 1996
24
Ambient Noise Measurements
Paul C. Etter, Underwater Acoustic
Modeling, E & F SPON,
New York, NY, Second Edition, 1996
25
Directionality of Ambient Noise
26
Ambient Noise Near Compact Ice Edge
27
Radar Equation Definitions
SNR = Signal-to-noise ratio
PT = Transmitter power
GT = Transmitter directional gain
r = Range to target
= Attenuation coefficient
= Effective target scattering cross-section
AR = Effective area of receiver
KBT = Thermal noise power
Pamb = Ambient noise power
Prev = Reverberation backscattered power
Convert equation to dB by taking 10 log of both sides of
the equation.
28
The Radar/Sonar Equation
SNR = Signal Power
Noise Power
= Gain Against Noise or reverberation
29
Sonar Equations (dB Values)
Active Sonar – Ambient Noise Background
[SL - 2TL - + TS] = [NL – DT] + DT + SE
Active Sonar – Reverberation Background
[SL - 2TL - + TS] = (RL) + DT + SE
Passive Sonar
[SL - TL] = (NL – DI) + DT + SE
Signal Level = Effective + Required + Signal
Masking Signal Excess
Noise to Noise Relative
Ratio to DT
30
Solving the Sonar Equation
The sonar equation expresses the signal-to-noise
ration as function of the sonar and environmental
parameters. At the maximum detection range, the
received signal power divided by the noise power is
equal to the detection threshold. (Signal excess is
zero.) Uncertainties in some of the parameters,
especially TL and NL, limit the accuracy of prediction
to a few dB.
31
Figure of Merit
FOM equals the maximum allowable one-way transmission
loss in passive sonar or the maximum allowable two-way
transmission in active sonar.
Passive FOM = TL = SL - [NL – DI + DT]
Active FOM = 2TL = SL + TS – [NL – DI + DT]
Note:
Including TS in active FOM disagrees with Urick, but is a
common practice.
FOM is not useful for reverberation limited ranges.
32
Passive Sonar Prediction
[SL – TL] - [NL – DI] = DT
Received - Background = Detection
Signal Level Masking Noise Threshold
Urick [75]
33
Active Sonar Prediction
Urick [75]
34
Active Sonar Parameters
Parameter Symbol Important Factors
Source Level SL Input Power
Conversion Efficiency
Directivity Index
Cavitation Limitations
Target Strength TS Target Area
Target Aspect
Pulse Duration
Frequency
Reverberation Level RL Source Level
Beam Width
Pulse Length
Boundaries
Scattering Layers
Frequency
35
Detection Threshold
DT = 10 log Req Signal Power for a Spec. Performance
Noise Power per Hz at the Receiver Input
Detection Threshold (DT) is defined as the ratio (in decibels) of
the signal power in the receiver bandwidth to the noise ower
spectrum level (in a 1 Hz band) measured at the receiver
terminals, required for detection at some specified level of
correctness of the detection decision [i.e., p(D) and p(FA)].
Typical requirements per decision (or per look):
p(D) = 0.5 or 0.9
p(FA) = 10-6
Urick [75]
36
Detection Decision
Decide “Signal Present” when the input exceeds the expected value of
noise by more than a bias level; otherwise, decide “Signal Absent.”
Decision
True Input
Signal Present Signal Absent
Signal Present Correct
DETECTION p(D)
False Dismissal
1-p(D)
Signal Absent FALSE Alarm
p(FA)
Correct Dismissal
1-p(FA)
Urick [75]
37
Signal Detection Experiment
GAUSSIAM NOISE GENERATOR
Average noise level N
15-second sections
STEADY SINUSOIDAL SIGNALS
Duration T
Average Power S
THE EXPERIMENT
Signals embedded in half the 15-second noise sections
(or echo cycles)
Listeners push button when “signal present”
LISTENER TRAINING
Easily detected signals
Signal levels gradually reduced
38
Data Collection
• “HIT” SCORED WHEN LISTENER RESPONDED
WITHIN 1 SEC. AFTER SIGNAL OCCURRENCE
• “FALSE ALARM” SCORED WHEN LISTENER
RESPONDED TO NOISE
• LISTENERS WERE NOT RESTRICTED TO ONE
RESPONSE PER NOISE SECTION
• SCORES WERE TABULATED USING LAST
RESPONSE IN EACH SECTION
39
Estimates of PD and PFA
PD = ____________NUMBER OF “HITS” ___________________
NUMBER OF NOISE SECTIONS WITH SIGNALS
PFA = NUMBER OF “EMPTY SECTIONS” IN WHICH RESPONSES WERE MADE
NUMBER OF “EMPTY” NOISE SECTIONS
“EMPTY” NOISE SECTION IS NOISE SECTION WITH NO EMBEDDED SIGNAL.
40
Experiment Results
♦LISTENED TO SEVERAL HUNDRED NOISE SECTIONS
•Different days
•Different instructions on strictness about responding
♦PD PLOT AGAINST PFA GROUPED AROUND THEORETICALLY COMPUTED S = 0 dB Curve
N
♦WHEN AVERAGE S/N CHANGED TO ±2 dB, MEASUREMENTS CLUSTERED
AROUND S/N = ±2dB CURVES, ETC.
NOTE: log10(1) = 0 means <S> = <N>
Receiving Operating Characteristics (ROC) Operating Curves
41
42
Interpretation of Results
• PD increases with S/N
• PFA decreases as S/N increases
• Visual detection
– Noise sections written out as pen recordings (such as
time bearing plots)
– Observers detect signal by viewing recorder plots
– Different set of PD vs. PFA curves
– Eye not as good (for detection) as ead
43
Concept Leading to Construction of ROC Curves
Output Levels:
•Energy detector – Mean square amplitude of power
•Voltmeter
•Oscillate about (B) when no signal present
•Oscillate about (A) when signal present
44
Gaussian Distribution (Model of Random Noise)
Central Limit Theorem: The random selection of values from any
distribution (Gaussian or not) tends to a Gaussian distribution with the same
mean and standard deviation as was in the original distribution.
45
Normal Distribution Probability Density and Cumulative
Distribution Functions
Cumulative Distribution FunctionNormal Distribution Density
46
Normal Bell-Shaped Curve
47
Computing ROC Curves
DETECTABILITY
INDEX:
P(y/N) = Prob. Density of output y, given N as input
P(y/SN) = Prob. Density of output y, given S+N as input
IDEAL ENERGY DETECTOR
E = Total signal energy received during time T in band W
S = Signal power in band W (note: E = ST)
T = Sample time of detector
W = Input bandwidth of the detector system
48
Evaluation of P(D) and P(F)
(Prob. density of noise)
(Prob. density of signal and noise)
49
ROC Curves for an Energy Detector
50
Required signal-to-noise (visibility factor) at the input terminals of a linear-rectifier
detector as a function of probability of detection for a single pulse, with the false-alarm
probability (PFA) as a parameter, calculated for a non-fluctuating signal
Blake [69]
Visibility Factor (Radar)
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Sonar Principles Asw Analysis

  • 1. 1 Lecture I The Sonar Equation and Signal Detection Dr. Nicholas C. Nicholas Applied Technology Institute 349 Berkshire Drive Riva, Maryland 21140 888-501-2100/410-956-8805 Website: www.ATIcourses.com Email: ATI@ATIcourses.com ATI Course Schedule: http://www.ATIcourses.com/schedule.htm ATI’s IP Networking Over Satellite: http://www.aticourses.com/sonar_principles_asw_analysis.htm
  • 2. 10 – Vol. 95 Register online at www.ATIcourses.com or call ATI at 888.501.2100 or 410.956.8805 Sonar Principles & ASW Analysis Off The Course Tuition." Summary This course provides an excellent introduction to underwater sound and highlights how sonar principles are employed in ASW analyses. The course provides a solid understanding of the sonar equation and discusses in- depth propagation loss, target strength, reverberation, arrays, array gain, and detection of signals. Physical insight and typical results are provided to help understand each term of the sonar equation. The instructors then show how the sonar equation can be used to perform ASW analysis and predict the performance of passive and active sonar systems. The course also reviews the rationale behind current weapons and sensor systems and discusses directions for research in response to the quieting of submarine signatures. The course is valuable to engineers and scientists who are entering the field or as a review for employees who want a system level overview. The lectures provide the knowledge and perspective needed to understand recent developments in underwater acoustics and in ASW. A comprehensive set of notes and the textbook Principles of Underwater Sound will be provided to all attendees. Instructors Dr. Nicholas Nicholas received a B. S. degree from Carnegie-Mellon University, an M. S. degree from Drexel University, and a PhD degree in physics from the Catholic University of America. His dissertation was on the propagation of sound in the deep ocean. He has been teaching underwater acoustics courses since 1977 and has been visiting lecturer at the U.S. Naval War College and several universities. Dr. Nicholas has more than 25 years experience in underwater acoustics and submarine related work. He is working for Penn State’s Applied Research Laboratory (ARL). Dr. Robert Jennette received a PhD degree in Physics from New York University in 1971. He has worked in sonar system design with particular emphasis on long- range passive systems, especially their interaction with ambient noise. He held the NAVSEA Chair in Underwater Acoustics at the US Naval Academy where he initiated a radiated noise measurement program. Currently Dr. Jennette is a consultant specializing in radiated noise and the use of acoustic monitoring. Course Outline 1. Sonar Equation & Signal Detection. Sonar concepts and units. The sonar equation. Typical active and passive sonar parameters. Signal detection, probability of detection/false alarm. ROC curves and detection threshold. 2. Propagation of Sound in the Sea. Oceanographic basis of propagation, convergence zones, surface ducts, sound channels, surface and bottom losses. 3. Target Strength and Reverberation. Scattering phenomena and submarine strength. Bottom, surface, and volume reverberation mechanisms. Methods for modeling reverberations. 4. Elements of ASW Analysis. Fundamentals of ASW analysis. Sonar principles and ASW analysis, illustrative sonobuoy barrier model. The use of operations research to improve ASW. 5. Arrays and Beamforming. Directivity and array gain; sidelobe control, array patterns and beamforming for passive bottom, hull mounted, and sonobuoy sensors; calculation of array gain in directional noise. 6. Passive Sonar. Illustrations of passive sonars including sonobuoys, towed array systems, and submarine sonar. Considerations for passive sonar systems, including radiated source level, sources of background noise, and self noise. 7. Active Sonar. Design factors for active sonar systems including transducer, waveform selection, and optimum frequency; examples include ASW sonar, sidescan sonar, and torpedo sonar. 8. Theory and Applications of Current Weapons and Sensor Systems. An unclassified exposition of the rationale behind the design of current Navy acoustic systems. How the choice of particular parameter values in the sonar equation produces sensor designs optimized to particular military requirements. Generic sonars examined vary from short-range active mine hunting sonars to long-range passive systems. What You Will Learn • Sonar parameters and their utility in ASW Analysis. • Sonar equation as it applies to active and passive systems. • Fundamentals of array configurations, beamforming, and signal detectability. • Rationale behind the design of passive and active sonar systems. • Theory and applications of current weapons and sensors, plus future directions. • The implications and counters to the quieting of the target’s signature. SEE CURRENT SCHEDULE FOR THE LATEST DATES http://www.ATIcourses.com/schedule.htm
  • 3. www.ATIcourses.com Boost Your Skills with On-Site Courses Tailored to Your Needs The Applied Technology Institute specializes in training programs for technical professionals. Our courses keep you current in the state-of-the-art technology that is essential to keep your company on the cutting edge in today’s highly competitive marketplace. Since 1984, ATI has earned the trust of training departments nationwide, and has presented on-site training at the major Navy, Air Force and NASA centers, and for a large number of contractors. Our training increases effectiveness and productivity. Learn from the proven best. For a Free On-Site Quote Visit Us At: http://www.ATIcourses.com/free_onsite_quote.asp For Our Current Public Course Schedule Go To: http://www.ATIcourses.com/schedule.htm 349 Berkshire Drive Riva, Maryland 21140 Telephone 1-888-501-2100 / (410) 965-8805 Fax (410) 956-5785 Email: ATI@ATIcourses.com
  • 4. 2 What is Sound? Sound is a mechanical wave motion propagating in an elastic medium. Associated with this wave motion are changes in the local pressure and density. Sonar, an acronym for SOund NAvigation and Ranging, uses sound energy (generally underwater) to transmit information.
  • 5. 3 Longitudinal Waves COMPRESSIONS AND RAREFACTIONS OF LONGITUDINAL WAVES λ = WAVELENGTH f = FREQUENCY c = SPEED OF SOUND
  • 6. 4 Terminology Psycho/Physiological Physical Pitch Frequency (Nominal) Audible Range: 20 –20,000 Hz Speech Range : 100 – 4,000 Hz Infrasonic : Below audible range Ultrasonic : Above audible range Loudness Intensity Intensity = 10 LOG10 I1/I0 = 20 LOG10 P1/P0 Decibels (dB) Quality Waveform Spectrum, Relative amplitudes/phases
  • 7. 5 Nominal Speed of Sound Material Speed of Sound (m/s) Density (g/cm3) Aluminum (rolled) 6420 2.7 Stainless Steel 5790 7.9 Rubber, Gum 1550 0.95 Fresh Water (25oC) 1498 0.998 Sea Water (25oC) 1531 1.025 Air 331 0.0012 Sea Water 1430→1530
  • 8. 6 Acoustic Wavelength versus Frequency Wavelength = sound speed/ frequency λ = c/f
  • 9. 7 Sensitivity of the Human Ear 0 dB = 0.0002 dyne/ sq. cm Shortly & Williams (53)
  • 10. 8 Doppler Shift (Passive Sonar) When a sound source is moving with respect to an acoustic observer, the frequency of the sound is shifted. f0 = fs c + V0 c - Vs f0 = observed frequency fs = frequency at the source c = speed of sound V0 = speed of observer approaching sound source = V1 cos Θ Vs = speed of source approaching observer = V2 cos Θ Θ = bearing angle Doppler shift is about 0.35 Hz per knot, about 1% at 30 knots
  • 11. 9 Doppler Shift (Active Sonar) In active sonar, the approaching target received a signal which is shifted higher in frequency (up-Doppler), then reradiates as a moving source approaching the receiver, causing a doubling of the Doppler shift. f = 0.69 Hz/(knot) (KHz) [ACTIVE] REMEMBER Approaching target produces an up-Doppler. Receding target produced a down-Doppler. Active sonar Doppler shift is double that of passive sonar (about 2% at 30 knots)
  • 12. 10 Lofargram of Simulated Aircraft Overflight
  • 13. 11 Decibel (dB) Decibels are 10 times the logarithm (to base 10) of the ration of a power or power-related quantity divided by a reference level. I (dB re 1 watt/cm2) = 10 log I (watts/cm2) Iref (watt/cm2) Remember the following properties of logarithms: log 10X = X log [10X 10Y] = log 10(X+Y) = X+Y To convert from dB to linear units i (linear ratio) = 10(0.1)I Where i = linear ration normalized by reference unit I = dB value.
  • 14. 12 Intensity/Pressure/Acoustic Impedance Intensity is the (sound) power flow per unit area I = P2 / ρc where P = pressure amplitude ρc = acoustic impedance ρ = density c = speed of sound Intensity = 10 log I/Iref = 10 log (P/Pref )2 = 20 log P/P2
  • 15. 13 Pressure Units - Force per unit area - MKS units: 1 Pascal = 1 Newton/m2 - CGS units: 1 µbar = 1 dyne/cm2 -New reference unit 1 µPascal = 10-6 Newton/m2
  • 16. 14 Power Addition It is sometimes necessary to sum powers of two numbers which are expressed by dB. The numbers cannot be simply summed in dB form, as that would correspond to multiplication. In order to sum power, first convert from dB to the original units, add, and then express the result in dB. Alternately, the following curve can be used.
  • 17. 15 EXAMPLE FOR THE COMBINATION OF SHIPPING NOISE AND WIND WAVE NOISE EXAMPLE FOR DETECTION THRESHOLD = -5 dB (S/N)REQ = -5 dB [(S+N/N)]REQ = 1.2 dB
  • 18. 16 More Examples If the acoustic pressure in a plane wave is increased by a factor of 3, what is the change in level of the sound? If the acoustic intensity in a plane wave is increased by a factor of 3, what is the change in level of the sound? If the acoustic pressure in a plane wave is reduced to 1/4, what is the change in level of the sound? If the acoustic intensity in a plane wave is reduced to 1/10, what is the change in level of the sound?
  • 19. 17 Yet More Examples At a certain location the noise level due to oceanic turbulence is 70 dB, the noise level due to distant shipping is 73 dB, and the self-noise level is 73 dB. What is the total noise level?
  • 20. 18 Bathymetry Illustration of bathymetrically unimpeded ray paths emanating from Herd Islands with the indicated launch angles. All rays are refracted geodesics along the surface containing the sound channel axis. White boxes indicate locations of oceanographic research stations capable of receiving acoustic signals. (Munk and Forbes, 1989; J. Phys. Oceanography, No. 19, 1965-78; copyright by the American Meteorological Society)
  • 23. 21 Bathymetry and Sound Speed Structure
  • 24. 22 Ambient Noise Measurements Paul C. Etter, Underwater Acoustic Modeling, E & F SPON, New York, NY, Second Edition, 1996
  • 25. 23 Bathymetric and Sound Speed Structure (North Pacific) Paul C. Etter, Underwater Acoustic Modeling, E & F SPON, New York, NY, Second Edition, 1996
  • 26. 24 Ambient Noise Measurements Paul C. Etter, Underwater Acoustic Modeling, E & F SPON, New York, NY, Second Edition, 1996
  • 28. 26 Ambient Noise Near Compact Ice Edge
  • 29. 27 Radar Equation Definitions SNR = Signal-to-noise ratio PT = Transmitter power GT = Transmitter directional gain r = Range to target = Attenuation coefficient = Effective target scattering cross-section AR = Effective area of receiver KBT = Thermal noise power Pamb = Ambient noise power Prev = Reverberation backscattered power Convert equation to dB by taking 10 log of both sides of the equation.
  • 30. 28 The Radar/Sonar Equation SNR = Signal Power Noise Power = Gain Against Noise or reverberation
  • 31. 29 Sonar Equations (dB Values) Active Sonar – Ambient Noise Background [SL - 2TL - + TS] = [NL – DT] + DT + SE Active Sonar – Reverberation Background [SL - 2TL - + TS] = (RL) + DT + SE Passive Sonar [SL - TL] = (NL – DI) + DT + SE Signal Level = Effective + Required + Signal Masking Signal Excess Noise to Noise Relative Ratio to DT
  • 32. 30 Solving the Sonar Equation The sonar equation expresses the signal-to-noise ration as function of the sonar and environmental parameters. At the maximum detection range, the received signal power divided by the noise power is equal to the detection threshold. (Signal excess is zero.) Uncertainties in some of the parameters, especially TL and NL, limit the accuracy of prediction to a few dB.
  • 33. 31 Figure of Merit FOM equals the maximum allowable one-way transmission loss in passive sonar or the maximum allowable two-way transmission in active sonar. Passive FOM = TL = SL - [NL – DI + DT] Active FOM = 2TL = SL + TS – [NL – DI + DT] Note: Including TS in active FOM disagrees with Urick, but is a common practice. FOM is not useful for reverberation limited ranges.
  • 34. 32 Passive Sonar Prediction [SL – TL] - [NL – DI] = DT Received - Background = Detection Signal Level Masking Noise Threshold Urick [75]
  • 36. 34 Active Sonar Parameters Parameter Symbol Important Factors Source Level SL Input Power Conversion Efficiency Directivity Index Cavitation Limitations Target Strength TS Target Area Target Aspect Pulse Duration Frequency Reverberation Level RL Source Level Beam Width Pulse Length Boundaries Scattering Layers Frequency
  • 37. 35 Detection Threshold DT = 10 log Req Signal Power for a Spec. Performance Noise Power per Hz at the Receiver Input Detection Threshold (DT) is defined as the ratio (in decibels) of the signal power in the receiver bandwidth to the noise ower spectrum level (in a 1 Hz band) measured at the receiver terminals, required for detection at some specified level of correctness of the detection decision [i.e., p(D) and p(FA)]. Typical requirements per decision (or per look): p(D) = 0.5 or 0.9 p(FA) = 10-6 Urick [75]
  • 38. 36 Detection Decision Decide “Signal Present” when the input exceeds the expected value of noise by more than a bias level; otherwise, decide “Signal Absent.” Decision True Input Signal Present Signal Absent Signal Present Correct DETECTION p(D) False Dismissal 1-p(D) Signal Absent FALSE Alarm p(FA) Correct Dismissal 1-p(FA) Urick [75]
  • 39. 37 Signal Detection Experiment GAUSSIAM NOISE GENERATOR Average noise level N 15-second sections STEADY SINUSOIDAL SIGNALS Duration T Average Power S THE EXPERIMENT Signals embedded in half the 15-second noise sections (or echo cycles) Listeners push button when “signal present” LISTENER TRAINING Easily detected signals Signal levels gradually reduced
  • 40. 38 Data Collection • “HIT” SCORED WHEN LISTENER RESPONDED WITHIN 1 SEC. AFTER SIGNAL OCCURRENCE • “FALSE ALARM” SCORED WHEN LISTENER RESPONDED TO NOISE • LISTENERS WERE NOT RESTRICTED TO ONE RESPONSE PER NOISE SECTION • SCORES WERE TABULATED USING LAST RESPONSE IN EACH SECTION
  • 41. 39 Estimates of PD and PFA PD = ____________NUMBER OF “HITS” ___________________ NUMBER OF NOISE SECTIONS WITH SIGNALS PFA = NUMBER OF “EMPTY SECTIONS” IN WHICH RESPONSES WERE MADE NUMBER OF “EMPTY” NOISE SECTIONS “EMPTY” NOISE SECTION IS NOISE SECTION WITH NO EMBEDDED SIGNAL.
  • 42. 40 Experiment Results ♦LISTENED TO SEVERAL HUNDRED NOISE SECTIONS •Different days •Different instructions on strictness about responding ♦PD PLOT AGAINST PFA GROUPED AROUND THEORETICALLY COMPUTED S = 0 dB Curve N ♦WHEN AVERAGE S/N CHANGED TO ±2 dB, MEASUREMENTS CLUSTERED AROUND S/N = ±2dB CURVES, ETC. NOTE: log10(1) = 0 means <S> = <N>
  • 43. Receiving Operating Characteristics (ROC) Operating Curves 41
  • 44. 42 Interpretation of Results • PD increases with S/N • PFA decreases as S/N increases • Visual detection – Noise sections written out as pen recordings (such as time bearing plots) – Observers detect signal by viewing recorder plots – Different set of PD vs. PFA curves – Eye not as good (for detection) as ead
  • 45. 43 Concept Leading to Construction of ROC Curves Output Levels: •Energy detector – Mean square amplitude of power •Voltmeter •Oscillate about (B) when no signal present •Oscillate about (A) when signal present
  • 46. 44 Gaussian Distribution (Model of Random Noise) Central Limit Theorem: The random selection of values from any distribution (Gaussian or not) tends to a Gaussian distribution with the same mean and standard deviation as was in the original distribution.
  • 47. 45 Normal Distribution Probability Density and Cumulative Distribution Functions Cumulative Distribution FunctionNormal Distribution Density
  • 49. 47 Computing ROC Curves DETECTABILITY INDEX: P(y/N) = Prob. Density of output y, given N as input P(y/SN) = Prob. Density of output y, given S+N as input IDEAL ENERGY DETECTOR E = Total signal energy received during time T in band W S = Signal power in band W (note: E = ST) T = Sample time of detector W = Input bandwidth of the detector system
  • 50. 48 Evaluation of P(D) and P(F) (Prob. density of noise) (Prob. density of signal and noise)
  • 51. 49 ROC Curves for an Energy Detector
  • 52. 50 Required signal-to-noise (visibility factor) at the input terminals of a linear-rectifier detector as a function of probability of detection for a single pulse, with the false-alarm probability (PFA) as a parameter, calculated for a non-fluctuating signal Blake [69] Visibility Factor (Radar)
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