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Kobernichenko V.G. (1), kand. tech. sci. (PhD), professor;
Sosnovsky A.V. (1), sen. engineer; Vinogradova N.S. (1), sen. lecturer;
Tsogtbaatar O. (1,2), jun. scientist
(1)IRIT-RTF UrFU, Ekaterinburg
(2) Ulan-Baator tech. univ., Mongolia
InSAR data coherence estimation using 2D
fast Fourier transform
InSAR signals coherence
(ALOS PALSAR data)
low
high
mediate
coherence map interferogram
Coherence map application
 damaged areas rejection for subsequent InSAR
processing steps facilitation;
 as a parameter for adaptive phase noise
suppression methods (i.e. Goldstein-Baran
spectral filter);
 territories classification.
Coherence estimates
1 2
0 2 2
1 2
( , ) ( , )
ˆ
( , ) ( , )
z i j z i j
z i j z i j
γ
×
=
×
∑
∑ ∑
&
- standard estimate
1 2
3 2 2
1 2
( , ) ( , )
ˆ
( , ) ( , )
w i j w i j
w i j w i j
γ
×
=
×
∑
∑ ∑
&
& &
1,2 1,2 1,2( , ) ( , ) ( 1, 1)w i j z i j z i j= × − −& &,
( , )
1 2
2 2 2
1 2
( , ) ( , )
ˆ
( , ) ( , )
jФ i j
z i j z i j e
z i j z i j
γ
−
× ×
=
×
∑
∑ ∑
)
&
- estimated topographic phase (from
an external data source)
( , )Ф i j
)
,
Coherence estimate degradation caused by phase
slope
0 20 40 60 80 100
-2
0
2
0 20 40 60 80 100
-2
0
2
0 20 40 60 80 100
-2
0
2
0
ˆ 0.99γ =
0
ˆ 0.80γ =
0
ˆ 0.21γ =
0
ˆγ
Coherence estimate degradation
caused by phase slope
0 50 100 150 200 250 300 350
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 50 100 150 200 250 300 350
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
With the fixed window size(N=10) With the fixed correlation coefficient
(r=0.7)
0
ˆγ
angle
N=3,10,25
angle
estimate
( , )
1 2
4 2 2
1 2
( , ) ( , )
ˆ
( , ) ( , )
jФ i j
c c
c c
z i j z i j e
z i j z i j
γ
−
× ×
=
×
∑
∑ ∑
)
&
{ }( )
0
0
2
1 2( , ) arg max ( , ) ( , )
i i N
j j M
Ф i j F z i j z i j
≤ ±
≤ ±
= ×
)
&
- topographic phase slope estimate in MxN sample window( , )Ф i j
)
4
ˆγ
- normalized SAR images amplitudesiici zzz &&& /=
Phase slope correction in spectral domain
( , ) x y
i j
j
jФ i j M N
e e
ω ω
 
− × + × −  
× =
)
0
N/2=1, 2, 5, 10, 25
2FFT spectrum peak-to mean ratios
with different window sizeswith different signal correlation
coefficients
0,2
0,5
0,8
1,0
N/2 ρ&
2FFT peak-to-mean ratio (N+1)x(N+1) window sizes
and comparison
X-band SAR data scenes
2
ˆγ 4
ˆγ
SAR image №1 SAR image №2
0 2
ˆ ˆ( )γ γ 4
ˆγ
Coherence maps:
Estimate degradation:
«specks»
and comparison2
ˆγ 4
ˆγ
and comparison2
ˆγ 4
ˆγ
γ
σψ
γ
γ
4
2
radians
Phase accuracy dependence on the coherence value for both estimates

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InSAR Data Coherence Estimation Using 2D Fast Fourier Transform

  • 1. Kobernichenko V.G. (1), kand. tech. sci. (PhD), professor; Sosnovsky A.V. (1), sen. engineer; Vinogradova N.S. (1), sen. lecturer; Tsogtbaatar O. (1,2), jun. scientist (1)IRIT-RTF UrFU, Ekaterinburg (2) Ulan-Baator tech. univ., Mongolia InSAR data coherence estimation using 2D fast Fourier transform
  • 2. InSAR signals coherence (ALOS PALSAR data) low high mediate coherence map interferogram
  • 3. Coherence map application  damaged areas rejection for subsequent InSAR processing steps facilitation;  as a parameter for adaptive phase noise suppression methods (i.e. Goldstein-Baran spectral filter);  territories classification.
  • 4. Coherence estimates 1 2 0 2 2 1 2 ( , ) ( , ) ˆ ( , ) ( , ) z i j z i j z i j z i j γ × = × ∑ ∑ ∑ & - standard estimate 1 2 3 2 2 1 2 ( , ) ( , ) ˆ ( , ) ( , ) w i j w i j w i j w i j γ × = × ∑ ∑ ∑ & & & 1,2 1,2 1,2( , ) ( , ) ( 1, 1)w i j z i j z i j= × − −& &, ( , ) 1 2 2 2 2 1 2 ( , ) ( , ) ˆ ( , ) ( , ) jФ i j z i j z i j e z i j z i j γ − × × = × ∑ ∑ ∑ ) & - estimated topographic phase (from an external data source) ( , )Ф i j ) ,
  • 5. Coherence estimate degradation caused by phase slope 0 20 40 60 80 100 -2 0 2 0 20 40 60 80 100 -2 0 2 0 20 40 60 80 100 -2 0 2 0 ˆ 0.99γ = 0 ˆ 0.80γ = 0 ˆ 0.21γ = 0 ˆγ
  • 6. Coherence estimate degradation caused by phase slope 0 50 100 150 200 250 300 350 0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 0 50 100 150 200 250 300 350 0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1 With the fixed window size(N=10) With the fixed correlation coefficient (r=0.7) 0 ˆγ angle N=3,10,25 angle
  • 7. estimate ( , ) 1 2 4 2 2 1 2 ( , ) ( , ) ˆ ( , ) ( , ) jФ i j c c c c z i j z i j e z i j z i j γ − × × = × ∑ ∑ ∑ ) & { }( ) 0 0 2 1 2( , ) arg max ( , ) ( , ) i i N j j M Ф i j F z i j z i j ≤ ± ≤ ± = × ) & - topographic phase slope estimate in MxN sample window( , )Ф i j ) 4 ˆγ - normalized SAR images amplitudesiici zzz &&& /=
  • 8. Phase slope correction in spectral domain ( , ) x y i j j jФ i j M N e e ω ω   − × + × −   × = )
  • 9. 0 N/2=1, 2, 5, 10, 25 2FFT spectrum peak-to mean ratios with different window sizeswith different signal correlation coefficients 0,2 0,5 0,8 1,0 N/2 ρ& 2FFT peak-to-mean ratio (N+1)x(N+1) window sizes
  • 10. and comparison X-band SAR data scenes 2 ˆγ 4 ˆγ SAR image №1 SAR image №2
  • 11. 0 2 ˆ ˆ( )γ γ 4 ˆγ Coherence maps: Estimate degradation: «specks» and comparison2 ˆγ 4 ˆγ
  • 12. and comparison2 ˆγ 4 ˆγ γ σψ γ γ 4 2 radians Phase accuracy dependence on the coherence value for both estimates