Upload
others
View
7
Download
0
Embed Size (px)
Citation preview
Robust Range-rate Estimation of Passive Narrowband Sources inShallow Water
Hailiang Tao and Jeffrey Krolik
Department of Electrical and Computer Engineering
Duke University
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 1/23
Outline
• Introduction• The Independent Mode Range-rate Estimator• Comparison with Cramer-Rao Bound• Application to SWellEx-96 data• Conclusions.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 2/23
Range-Rate Discrimination in Passive Sonar
Motivation:• Range-rate is a more robust searching dimension with regard to
wavenumber mismatch in Matched Field Processing (MFP) comparedwith absolute range.
• The discrimination capability in range-rate is helpful to detect targets inthe presence of interferences with similar bearings but different relativerange-rate.
Background:
• Normal mode theory for a narrowband moving source derived byHawker (JASA, 1979). Projection of target Doppler onto different modesinduces signal fluctuations which are target range-rate dependent.
• Direct application of MUSIC (Song, 1990) does not take advantage ofavailable environmental information and requires a long observationtime.
• Direct extension of Matched Field Processing (Zala, 1992) with range-rateis computational intensive due to parameter coupling.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 3/23
Acoustic Normal Mode Theory For a Moving Source
The velocity potential emitted by a narrowband, horizontally uniform movingpoint source, in a range-independent stratified oceanic waveguide: (Hawker,1979)
ψ(t) ≈ CM
X
m=1
Um(z)Um(zs)√kmR0
exp
»
jωmt− jkmR0„
1 − vrvGm
«–
(1)
where Um(z) and Um(zs) are mode eigenfunctions at receiver depth z andsource depth zs. km is the horizontal wavenumber. R0 the initial range.
ωm = ω0 − kmvr(1 −vrvGm
) ≈ ω0 − kmvr
is the Doppler frequency, in which ω0 is the intrinsic frequency, vr therange-rate of the source and vGm the group velocity of mode m.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 4/23
Differential Doppler for a Moving Source
Differential Doppler for moving vs. stationary source evident from slope offrequency distribution as a function of modal wavenumber for a single tonalsource. Note that range-rate dependence does not require relative phasebetween modal components.
0.15 0.16 0.17 0.18 0.19 0.2 0.21 0.22
47.5
48
48.5
49
49.5
50
50.5
Horizontal wavenumber (1/m)
Fre
quen
cy (
Hz)
f−k diagram for stationary and moving source
v=10m/sv=0
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 5/23
The Time-Frequency Data Snapshot Vector
Consider snapshot of narrowband data which consists of a concatenation of Nconventional frequency domain snapshots over time.
Note range-rate processing can be performed before or after conventionalbeamforming.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 6/23
The Signal Model (1)
Model the (pN × 1) space-time snapshot r as:
r = sX
m
am(dm ⊗ um) + n (2)
Where s is the signal amplitude, unknown nonrandom. am is a zero-meancomplex random variable representing mode m’s amplitude. dm is a timeharmonic vector for mode m:
dm = [1 e−jkmvrTd e−jkmvr2Td · · · e−jkmvr(N−1)Td ]T
⊗ is the Kronecker product. um represents mth mode eigenfunctionsevaluated at the depths of each array element:
um = [Um(z1) Um(z2) . . . Um(zp)]T
and n ∼ CN(0, σ2nI) represents complex white Gaussian noise.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 7/23
The Signal Model (2)
In matrix formr = sDa + n (3)
whereD = [d1 ⊗ u1 d2 ⊗ u2 . . . dM ⊗ uM ]
anda = [a1 a2 . . . aM ]
T
The variance of mode amplitude is
σ2m = E(amaHm) = Um(zs)
2/km (4)
In this model:• Assume am and an are uncorrelated for m 6= n.• The model is independent of absolute range.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 8/23
The Independent Mode Range-rate Estimator (IMRE)
The covariance matrix is:
R = E(rrH) = PsDSDH + σ2nI (5)
where Ps = |s|2 and S = E(aaH) = diag[σ21 σ22 . . . σ2M ].Given the environment and target depth zs, the signal covariance matrixRs = DSD
H could be computed for each hypothesized range-rate vr .Suppose the dominant eigenvector of Rs is h1 (normalized), then a Bartletttype estimator can be expressed as:
P (vr) =1
λ1h
H1 R̂h1 (6)
which maximizes output SNR in white noise. R̂ is the sample covariancematrix and λ1 is the maximum eigenvalue of R̂.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 9/23
The SWellEx-96 Environment
Typical shallow water environmental profiles of SWellEx-96 are used insimulations:
1485 1490 1495 1500 1505 1510 1515 1520 1525
0
20
40
60
80
100
120
140
160
180
200
216.5
Sound Velocity (m/s)
Dep
th (
m)
S5S59
SWellEx-96 Water Column SoundVelocity Profile
SWellEx-96 Sea Bottom Properties
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 10/23
Typical IMRE Output
−6 −4 −2 0 2 4 6−35
−30
−25
−20
−15
−10
−5
0
Range−rate (m/s)
IMR
E o
utpu
t pow
er (
dB)
Swellex96−S5:ds=51.0m, f
s=50Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, T
d=1.0s, nSample=200, SNR=20dB
The sidelobe is 13dB down from the mainlobe.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 11/23
Typical Eigenspectrum of Covariance Matrix R
Same settings as previous slide without noise. Source is moving at 2.5m/s.
Eigenvalue number Eigenvalues (dB) Normalized eigenvalues1 −18.3 0.97022 −33.4 0.02973 −59.6 0.7231 × 10−44 −85.2 0.1998 × 10−65 −111.7 0.4465 × 10−96 −140.8 0.5507 × 10−127 - 08 - 0...
......
20 - 0
The dB difference between 1st and 2nd eigenvalues corresponds tomainlobe/sidelobe difference in previous slide.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 12/23
Range-rate Aliasing
Range-rate difference between grating lobes:
vgr ≈2π
k̄Td(7)
where k̄ is the mean value of km. Td is the snapshot delay.
−20 −15 −10 −5 0 5 10 15 20−14
−12
−10
−8
−6
−4
−2
0
Range−rate (m/s)
IMR
E o
utpu
t pow
er (
dB)
Swellex96−s5:ds=51.0m, f
s=50Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, nSample=200, SNR=0dB
Td = 2s
Td = 0.5s
Grating Lobe Distance vrg
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 13/23
Insensitivity to Target Depth
Range−rate (m/s)
Dep
th (
m)
Swellex96−s5:ds=51.0m, f
s=50Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, T
d=1.0s, nSample=200, SNR=0dB
−6 −4 −2 0 2 4 6
0
20
40
60
80
100
120
140
160
180
200
−12
−10
−8
−6
−4
−2
IMRE search in both depth and range-rate with one sensor
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 14/23
Cramer-Rao Low Bound (1)
• The unknown parameters are: Θ = (vr, Ps, σ2n)T .• each element of Fisher Information Matrix (FIM) could be represented by:
Jij = Nstr
»
R−1 ∂R
∂θiR
−1 ∂R
∂θj
–
(8)
where Ns is the number of sampled r.To compute Jij , recall
R = PsDSDH + σ2nI
So∂R
∂Ps= DSDH (9)
∂R
∂σ2n= I (10)
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 15/23
Cramer-Rao Low Bound (2)
Let c = [0 1 2 . . . (N − 1)]T and k = [k1 k2 . . . kM ]T .Define matrix G:
G = −jTdckT
andH = G ⊗ h
where vector h is a p (array length) by 1 vector with all its elements being 1.Thus
∂R
∂vr= Ps(
∂D
∂vrSD
H + DS∂DH
∂vr)
= Ps((H � D)SDH + DS(H � D)H) (11)
where � is element-by-element Hadamard product.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 16/23
Comparison of IMRE with CRB
−20 −15 −10 −5 0 5−50
−40
−30
−20
−10
0
10
20
SNR(dB)
Ran
ge−
rate
MS
E (
dB)
Swellex96−S5: ds=51.0m, f
s=100Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, nSample=200, NMC=200
Monte CarloCRLB
Between SNR −15 ∼ 0dB, the mean square error of IMRE achieves CRLB. Thethreshold happens at −16dB.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 17/23
High SNR Behaviour Analysis
Express the dominant eigenvector of the sample covariance matrix as:
b̂1 = b1 + η (12)
The estimator error vector η has the following asymptotic correlation function:
E[ηηH ] =λ1Ns
NX
k=2
λk(λ′1 − λ′k)2
bkbHk
where λ′s are the eigenvalues of PsDSDH . Looking at λ1λk(λ′1−λ′
k)2
, we have:
• When the noise variance σ2n is far smaller than the second eigenvalue λ′2of PsDSDH , the performance of the algorithm will not improve withhigher SNR, i.e., not stick to the CRB.
• The smallest MSE achieveable is determined by λ′
2
λ′1
.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 18/23
High SNR Performance at Different Frequencies
0 5 10 15 20 25 30 35 40 45−55
−50
−45
−40
−35
Ran
ge−
rate
MS
E (
dB) Swellex96:ds=51.0m, fs=20Hz, vs=2.50m/s, da=70.0m, nsnap=20, nSample=200, NMC=200
0 5 10 15 20 25 30 35 40 45−55
−50
−45
−40
−35
Ran
ge−
rate
MS
E (
dB)
Swellex96:ds=51.0m, f
s=50Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, nSample=200, NMC=200
0 5 10 15 20 25 30 35 40 45−55
−50
−45
−40
−35
SNR(dB)
Ran
ge−
rate
MS
E (
dB)
Swellex96:ds=51.0m, f
s=100Hz, v
s=2.50m/s, d
a=70.0m, n
snap=20, nSample=200, NMC=200
λ’2/λ’
1 = 0.0018
λ’2/λ’
1=0.0306
λ’2/λ’
1=0.1096
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 19/23
Source Tracks in the SWellEx-96 Experiment
Source: UCSD Marine Physical Laboratory SWellEx-96 Website.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 20/23
Range-rate Track of S5 and S59 Events in SWellEx96
Time (m)
Ran
ge−
rate
(m
/s)
SwellEx96:s59 79Hz, zs=54.0m, z
a=94.1m, nSnap=20, t
FFT=1.0s
10 20 30 40 50 60−6
−4
−2
0
2
4
6
−40
−30
−20
−10
0
Time (m)
Ran
ge−
rate
(m
/s)
SwellEx96:s5 79Hz, zs=54.0m, z
a=94.1m, nSnap=20, t
FFT=1.0s
10 20 30 40 50 60 70−6
−4
−2
0
2
4
6
−40
−30
−20
−10
0
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 21/23
Summary and Comments
• A narrowband range-rate estimator, IMRE, is proposed. The methodexploits existing environmental information to obtain a more robust andaccurate estimation of range-rate.
• The aliasing and robustness of IMRE are discussed.• The performance of IMRE is compared favorably with Cramer-Rao
Lower Bound. The high SNR behavior is analysized.• Application of IMRE to the SWellEx-96 data set illustrates the practical
usage of the algorithm. Note in application of IMRE to real data, thedemodulation of FFT will introduce a bias, which will be addressed infuture research.
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 22/23
Thank You!
Robust Range-rate Estimation of Passive Narrowband Sources in Shallow Water – p. 23/23
OutlineRange-Rate Discrimination in Passive SonarAcoustic Normal Mode Theory For a Moving SourceDifferential Doppler for a Moving SourceThe Time-Frequency Data Snapshot VectorThe Signal Model (1)The Signal Model (2)The Independent Mode Range-rate Estimator (IMRE)The SWellEx-96 EnvironmentTypical IMRE OutputTypical Eigenspectrum of Covariance Matrix $R$Range-rate AliasingInsensitivity to Target DepthCramer-Rao Low Bound (1)Cramer-Rao Low Bound (2)Comparison of IMRE with CRBHigh SNR Behaviour AnalysisHigh SNR Performance at Different FrequenciesSource Tracks in the SWellEx-96 ExperimentRange-rate Track of S5 and S59 Events in SWellEx96Summary and Comments