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Article

A Modification to Phase Estimation for Distributed Scatterers in InSAR Data Stacks

1
School of Resources and Environment, University of Electronic Science and Technology of China, Chengdu 611731, China
2
Northwest Land and Resources Research Center, Shaanxi Normal University, Xi’an 710119, China
3
School of Earth Sciences and Spatial Information Engineering, Hunan University of Science and Technology, Xiangtan 411201, China
4
Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China
5
School of Civil Engineering and Geomatics, Southwest Petroleum University, Chengdu 610500, China
*
Author to whom correspondence should be addressed.
Remote Sens. 2023, 15(3), 613; https://doi.org/10.3390/rs15030613
Submission received: 11 December 2022 / Revised: 12 January 2023 / Accepted: 14 January 2023 / Published: 20 January 2023

Abstract

:
To improve the spatial density and quality of measurement points in multitemporal interferometric synthetic aperture radar, distributed scatterers (DSs) should be processed. An essential procedure in DS interferometry is phase estimation, which reconstructs a consistent phase series from all available interferograms. Influenced by the well-known suboptimality of coherence estimation, the performance of the state-of-the-art phase estimation algorithms is severely degraded. Previous research has addressed this problem by introducing the coherence bias correction technique. However, the precision of phase estimation is still insufficient because of the limited correction capabilities. In this paper, a modified phase estimation approach is proposed. Particularly, by incorporating the information on both interferometric coherence and the number of looks, a significant bias correction to each element of the coherence magnitude matrix is achieved. The bias-corrected coherence matrix is combined with advanced statistically homogeneous pixel selection and time series phase optimization algorithms to obtain the optimal phase series. Both the simulated and Sentinel-1 real data sets are used to demonstrate the superiority of this proposed approach over the traditional phase estimation algorithms. Specifically, the coherence bias can be corrected with considerable accuracy by the proposed scheme. The mean bias of coherence magnitude is reduced by more than 29%, and the standard deviation is reduced by more than 18% over the existing bias correction method. The proposed approach achieves higher accuracy than the current methods over the reconstructed phase series, including smoother interferometric phases and fewer outliers.

1. Introduction

Multitemporal interferometric synthetic aperture radar (MT-InSAR) is a powerful technique in monitoring the displacement of Earth’s surface [1,2,3], including a wide range of applications, such as land subsidence [4,5,6], underground mining [7,8], landslide [9,10,11], earthquake [12,13,14], volcanic dynamics [15,16,17] et al. Among various MT-InSAR techniques, the persistent scatterer InSAR (PSInSAR) is a high-precision geodetic approach [18,19]. The basic idea of this technique is to identify and analyze the phase-stable persistent scatterers (PSs) over the whole observation period. These scatterers do not undergo severe temporal decorrelation and usually correspond to man-made objectives. Despite the high precision of PSInSAR, the low spatial density of measurement points, especially over nonurban environments, limits its applications to some extent.
Distributed scatterers (DSs) are exploited to improve the measurement point density. Unlike PS, DS usually covers multiple small targets with the same backscattering behavior in a resolution cell. These targets suffer from geometrical and temporal decorrelation and are typically noisier than those of PSs. To reduce the decorrelation of DS, small baseline subset (SBAS) technique has been proposed by only exploiting interferograms with temporal intervals and spatial baselines smaller than the certain thresholds [20,21,22]. The decorrelation is further reduced by the spatial multi-looking processing. Since the PSs are also filtered with neighboring pixels, their backscattering properties may be contaminated.
To improve the measurement point density by jointly exploiting PSs and DSs, many efforts have been made [22,23,24,25,26], which can be broadly divided into two categories. One is to extend the SBAS technique by combining single-look and multi-look interferograms. PSs can be exploited to achieve fine-scale measurements [22,24]. The other is to extend the PSInSAR technique by adding DSs into the single-master model. The representative work is SqueeSAR [23], and some extended techniques include JSInSAR [27], CAESAR [28], PD-PSInSAR [29], GEOS-ATSA [30], CSI [9] et al. The decorrelation of DS can be significantly reduced by phase estimation.
Initially, the DS phase estimation was implemented based on a maximum likelihood estimator (MLE) [23,31,32], which reconstructs the consistent phase series by maximizing the joint probability density function (pdf) over all pixels in a statistically homogeneous pixel (SHP) set. Theoretically, MLE is the optimum approach for phase estimation. However, the assumptions are difficult to meet in practice, and the optimum performance is compromised. Then the variation is provided by the eigenvalue decomposition (EVD) algorithm [28,29]. Its advantage lies in separating multiple scattering mechanisms, and it has low power for a single scattering mechanism [33,34]. Recently, the eigen decomposition-based maximum-likelihood-estimator of interferometric phase (EMI) algorithm is provided [34]. It follows a similar estimation model as MLE, and has high computational efficiency. These estimators are mathematically compared, and the only difference is the weighting strategy [35]. Based on this, some estimators have been developed with different weights, such as the Fisher information index [36,37], equal weight [35], coherence weight [38,39], coherence power weight [40] et al.
Regardless of the model used by these phase estimation methods, the same data source is the covariance matrix, which is estimated by the maximum-likelihood estimation. As is well known, the estimation is suboptimal due to the heterogeneous samples and limited ensembles [41]. Recently, an alternative way is developed to mitigate the bias by jointly estimating the covariance matrix and the consistent phase series [42]. In general, these influencing factors are treated independently of the phase estimation. In terms of heterogeneous samples, advanced SHP selection algorithms have been developed to reduce the undesirable samples, such as probabilistic method [43], fast SHP selection (FaSHPS) [44], covariance matrix patch (CMP) [45] et al. Robust estimation has also been implemented to mitigate the impact of heterogeneous samples [46]. For limited ensembles, the corresponding covariance matrix usually does not satisfy the positive definiteness, which is required by some estimators for inverse matrix operation [23,34]. Regularization is exploited to solve this problem [47,48,49,50]. In addition, limited ensembles result in a biased covariance matrix, especially for low-coherence areas. The correction by inverting the analytical expression of the coherence magnitude can mitigate the bias [51]. Since the fixed rectangular window is used, the spatial resolution is reduced, and new bias may be introduced. The correction with the second kind of statistical characteristics is introduced to reduce the coherence magnitude bias [52] and shows promising performance [40,53,54]. However, compared with the true coherence, the improvement is inadequate due to the limited correction from a simple bias corrector [53]. Dedicated to accurate deformation monitoring, high-precision phase estimation is still lacking.
In this paper, a new approach is proposed to improve the accuracy of DS phase estimation for InSAR data stacks. Starting from the theoretical analysis of coherence magnitude matrix error, a systematic correction approach is developed by considering the information on both interferometric coherence and the number of looks. Besides, the CMP algorithm is adopted to select SHP set with a high detection rate, and the EMI is exploited to reconstruct the optimal phase series by combining the estimation and computational efficiency. The proposed approach is tested on both simulated and real Sentinel-1 data to demonstrate its effectiveness. The main contributions of this paper are as follows:
(1)
A bias corrector is developed to reduce the error of the coherence magnitude matrix.
(2)
The improvements in coherence bias correction for the state-of-the-art phase optimization algorithms are analyzed and evaluated.
(3)
A processing chain is provided to achieve the high-precision DS phase estimation.
This paper is organized as follows. In Section 2, the related methods are briefly reviewed, and the existing limitation is introduced. We then propose and elaborate on our approach in Section 3. Section 4 is dedicated to the presentation of the experimental results on simulated and real InSAR data stacks. Section 5 presents some discussions. Finally, conclusions are drawn in Section 6.

2. Related Method

Given N co-registered single-look complex (SLC) SAR images, a complex vector z ( x ) at the position x can be formed as
z ( x ) = [ z 1 ( x ) , z 2 ( x ) , , z N ( x ) ] T
where T denotes the transpose and z i ( x ) is the complex value of the i th acquisition at the position x .
Based on the central limit theorem, z follows a zero-mean N -variate complex circular normal distribution with a covariance matrix [55,56]. The pdf is
p d f ( z ) = 1 π N det ( ) exp ( z H 1 z )
where det ( ) indicates the determinant and H stands for Hermitian transpose. When z is normalized such that E ( | z i | 2 ) = 1 , the corresponding coherence matrix is equal to the covariance matrix [28] and can be estimated as
T ^ = 1 L k Ω z ( k ) z ( k ) H
where Ω is the SHP set with L adjacent pixels.
Although the phase of T ^ can be used for unwrapping and deformation retrieval, it is corrupted by the spatiotemporal decorrelation [23]. Phase optimization is developed to minimize the effect of decorrelation by properly combining the information associated with all the interferograms [23,31]. It supposes that the true coherence matrix can be expressed as
Σ = Ξ ϒ Ξ H
where
Ξ = [ e j θ 1 0 0 0 e j θ 2 0 0 0 e j θ N ]           ϒ = [ 1 γ 1 , 2 γ 1 , N γ 2 , 1 1 γ 2 , N γ N , 1 γ N , 2 1 ]
where Ξ and ϒ are the true phase and coherence magnitude matrix, respectively. Without loss of generality, θ 1 can be set to zero. Therefore, θ = [ 0 , θ 2 , , θ N ] T can be termed as the optimal phase series and needs to be estimated. The MLE obtains it by maximizing the joint pdf over all pixels in the SHP set Ω [23,31,32].
θ ^ M L E = arg max θ { k Ω p d f ( z k ) }               = arg max θ { ζ H ( ϒ 1 T ^ ) ζ }
where ζ = [ 1 , e j θ 2 , , e j θ N ] T and the symbol represents the Hadamard product. As the true coherence magnitude matrix ϒ is unknown, it is substituted by the absolute of T ^ .
θ ^ M L E = arg max θ { ζ H ( | T ^ | 1 T ^ ) ζ }
Equation (6) is a nonlinear optimization problem. Although the Broyden–Fletcher–Glodfarb–Shanno (BFGS) algorithm can be considered as a possible solution, the process is highly time-consuming [23].
Following the MLE, EMI is developed by introducing an additional degree of freedom with the calibration dyadic [34]. Besides, it transforms the nonlinear optimization problem into a minimum eigenvector problem.
θ ^ E M I = arg min u { u H ( | T ^ | 1 T ^ ) u }
where θ ^ = u , u is the eigenvector of | T ^ | 1 T ^ .
Compared with the MLE method, EMI is proven to be a more effective method, especially in terms of computational efficiency [34]. It is adopted in our proposed phase estimation algorithm, and the rationality can be found in Section 5.
As analyzed in [35], state-of-the-art phase estimation techniques adopt a similar mathematical model, such as MLE [23,31], EVD [28,29], EMI [34] and the nonlinear optimization estimation weighted with the Fisher information matrix (NLEFIM) [36]. The fundamental difference is the weight matrix, which assigns different weights to different interferograms. Furthermore, these weight strategies require the true coherence magnitude matrix ϒ , which is replaced by | T ^ | . As is well-known, Equation (3) is a suboptimal estimator, and the estimated coherence magnitude is biased [55]. The unsatisfactory factor makes the weight matrix inaccurate, resulting in severe damage to the accuracy of the estimated phase series θ ^ = [ 0 , θ ^ 2 , , θ ^ N ] T .

3. Methodology

In this section, the statistical characteristics of coherence magnitude bias are first analyzed. Then a systematic approach is developed to reduce the coherence bias. In the end, the bias-corrected coherence is combined with advanced SHP selection and phase optimization to obtain the consistent phase series.

3.1. Coherence Magnitude Bias Statistics

Let γ ^ be an element of the coherence magnitude matrix | T ^ | ; its pdf can be expressed as a function of the true coherence magnitude γ ; and the number of looks L as [57]
p d f ( γ ^ | γ , L ) = 2 ( L 1 ) ( 1 γ 2 ) L γ ^ ( 1 γ ^ 2 ) L 2 F 1 2 ( L , L ; 1 ; γ 2 γ ^ 2 )
where F is the generalized hypergeometric function. Based on the pdf, the analytical expression of the expectation and standard deviation of γ ^ can be derived as [58]
E ( γ ^ ) = Γ ( L ) Γ ( 3 / 2 ) Γ ( L + 1 / 2 ) F 2 3 ( 3 / 2 , L , L ; L + 1 / 2 , 1 ; γ 2 ) ( 1 γ 2 ) L    
D ( γ ^ ) = ( Γ ( L ) Γ ( 2 ) Γ ( L + 1 ) F 2 3 ( 2 , L , L ; L + 1 , 1 ; γ 2 ) ( 1 γ 2 ) L ( E ( γ ^ ) ) 2 ) 1 / 2
where Γ is the gamma function.
Equations (9) and (10) are calculated numerically. The difference between the expectation of sample coherence magnitude E ( γ ^ ) and true coherence γ is displayed in Figure 1a. It can be seen that the E ( γ ^ ) is biased towards higher values, and the bias increases with the decrease of γ and L . Figure 1b shows the standard deviation of sample coherence magnitude D ( γ ^ ) . It is clear that D ( γ ^ ) varies significantly with both γ and L . The lower the number of looks, the higher the standard deviation. Although the bias can be corrected by inverting Equation (9), the required condition with low D ( γ ^ ) , corresponding to a sufficiently large L , is difficult to meet in practice.
Based on the above analysis, a bias corrector should be designed with consideration of the differences at different coherence magnitudes and numbers of looks.

3.2. Bias Mitigation for Coherence Magnitude

The Mellin transform is a valuable tool to analyze the pdf defined on the positive real number field. Based on the second kind second characteristic function, the Mellin transform allows the second kind moment M s to follow the relation [52]
M s = 0 1 ( ln ( γ ^ ) ) s p d f ( γ ^ | γ , L ) d γ ^
The above equation can also be termed as log moment E ( ( ln ( γ ^ ) ) s ) . Thus, by inverting Equation (11), an estimator with the corrected coherence magnitude γ ˜ can be theoretically obtained as
γ ˜ = exp ( ( 1 ) s + 1 ( M s ) 1 / s )
Section 3.1 shows that the bias of sample coherence magnitude γ ^ is related to true coherence magnitude γ and the number of looks L . Here, the two factors are also considered. Based on the numerical calculation, the difference between the estimated coherence magnitude γ ˜ and true coherence magnitude γ is plotted in Figure 2. It can be seen that the value of s has an important influence on the bias of the estimated γ ˜ . In general, to obtain a more accurate γ ˜ , s should be assigned a larger value when the true coherence γ is lower and the number of looks L is smaller. Thus, the value of s should be assigned carefully. Besides, when the parameter is set to the constant s = 1 , the estimator (12) shares a simple form and is previously tested in [40,53,54]. In this paper, it is denoted by γ ¯ and is considered for comparison in the experimental section.
As the integral of Equation (11) is difficult to realize in practice, the log moment can be approximated by a statistical average over a large number of independent samples. Here, the SHP set Ω is used to ensure that the samples are independent and identically distributed. The log moment can be approximated as
M s 1 L k Ω ( ln ( γ ^ ( k ) ) ) s
From the qualitative analysis in Figure 2, we know that s should be assigned a value that is inversely proportional to both the true coherence magnitude γ and the number of looks L . To obtain a quantified solution formula for s , the values of γ , L and s are differentiated over a large range into small intervals. The theoretical γ ˜ is numerically calculated using Equations (11) and (12). Aiming at the minimum difference between γ ˜ and γ , the optimal s can be determined as
s = { 1 γ L > 5 [ 7 γ L ] 1 < γ L 5 6 γ L 1
where [ ] rounds down to an integer. Although s should be assigned a larger value when γ L 1 , the upper limit is set to 6 with the consideration of the limited accuracy improvements from larger values. In general, the number of looks L is not equal to the sample number. As Equation (14) is an approximate relationship and is not strict, the number of SHP set is used. The true coherence magnitude γ is unknown and needs to be estimated. Considering the variance of sample coherence magnitude γ ^ is relatively large, taking it as γ would result in an inaccurate s . Here, an empirical coherence magnitude is pre-estimated to replace γ .
Γ ^ = Γ ^ t h e r m a l Γ ^ g e o m Γ ^ t e m p
where
Γ ^ t h e r m a l = ( 1 + S N R 1 ) 1 Γ ^ g e o m = max ( 1 | B | / B max , 0 ) Γ ^ t e m p = exp ( B T / B T max ) }
where Γ ^ t h e r m a l is the thermal decorrelation, in which the signal-to-noise ratio (SNR) depends on system parameters and is usually assumed to be a constant value [58]. Γ ^ g e o m is the geometric decorrelation. B is the perpendicular baseline, and B max is the spatial decorrelation baseline, which corresponds to zero correlation [58]. Γ ^ t e m p is the temporal decorrelation, and the B T and B T max are the temporal baseline and decorrelation rate [58]. The three parameters, including S N R , B max and B T max , are specified in Section 4.1.
As the empirical coherence magnitude Γ ^ is a constant value for a single interferometric image, the sample coherence of each pixel can be appropriately corrected by different numbers of looks. The constant Γ ^ also ensures that the computational cost is not too high. In addition, the empirical coherence magnitude Γ ^ shares different values in different interferograms. For a single pixel, each element of | T ^ | can be corrected by the corresponding average coherence level. Therefore, the proposed algorithm can achieve effective correction for each element of all sample coherence magnitude matrices. In addition, compared to the sample coherence magnitude γ ^ using only SHPs within the search window, the proposed approach actually exploits more pixels, including not only those inside the search window but also those outside the window, which also contributes to reducing the bias of estimated coherence magnitude γ ˜ .

3.3. Phase Estimation Algorithm

Since the SHP set is not only used in Eqation (1) to estimate the sample coherence but also used in Equations (13) and (14) to correct the coherence magnitude bias, it requires to be identified precisely. The CMP algorithm exploits complex information and maintains high accuracy in different sizes of data stacks [45]. It is adopted in this paper to select SHPs.
f C M P ( x 1 , x 2 ) = exp ( 1 M i = 1 M 4 π ( I ^ 1 2 + I ^ 2 2 I ^ 1 I ^ 2 ( 1 T ^ i 2 cos ( ϕ ^ 1 , i ϕ ^ 2 , i ) 1 T ^ i 2 ) 2 ) )
where the subscripts 1 and 2 correspond to two pixels with a search window. M interferometric pairs are generated, and ϕ ^ i is the i th original interferometric phase. I ^ is the temporal mean intensity and can be estimated as I ^ = j = 1 N I j / N . T ^ = h Γ ^ is an empirical coherence, where h acts as a factor to balance Γ ^ and ϕ ^ i . Based on a pre-defined threshold, the homogeneity of two pixels can be judged by whether f C M P is greater than the threshold.
The whole procedure of the proposed phase estimation algorithm can be described as follows (see Figure 3).
(1)
Apply the CMP algorithm to select SHP set Ω for each image-pixel p .
(2)
Estimate the coherence matrix T ^ using the selected SHP set Ω and Equation (3).
(3)
Pre-estimate the empirical coherence magnitude Γ ^ based on the InSAR stack information and Equation (15).
(4)
Determine parameter s with empirical coherence magnitude Γ ^ , SHP set Ω and Equation (14).
(5)
Estimate the log moment M s using the sample coherence magnitude γ ^ , parameter s and Equation (13).
(6)
Calculate the corrected coherence magnitude γ ˜ with the log moment M s and Equation (12).
(7)
Reconstruct the consistent phase series using EMI and the bias-corrected coherence matrix.
Note that the proposed approach with coherence magnitude bias correction can be termed a general strategy and can be used in other DS phase estimators, such as MLE, EVD and NLEFIM. In practice, Equation (13) is calculated with a limited number of samples, which is generally difficult to meet the assumption of a large number of samples. Here, steps 5–6 are performed iteratively to mitigate this conflict. Considering a trade-off between accuracy improvement and computational cost increase, iteration is typically performed twice. When the computational cost is not considered, more iterations are recommended. In addition, the matrix inversion operation is required by EMI. For cases where the coherence matrix is not positive, definite regularization is committed to resolving the occasional problems via gradually adding a small negative eigenvalue of coherence [46].

4. Experimental Results

4.1. Test on Synthetic InSAR Data Stacks

The simulated data are synthesized based on the coherence matrix, in which the coherence magnitude can be derived as [59]
γ = ( γ 0 γ ) γ t h e r m a l γ g e o m γ t e m p + γ
where γ 0 and γ are the short-term and long-term coherence, and are set to 0.7 and 0.03, respectively. γ t h e r m a l , γ g e o m and γ t e m p are the thermal, geometric, and temporal decorrelation, and can be calculated using Equation (15). The SNR is set to 12 dB, resulting in γ t h e r m a l = 0.92 . The perpendicular baselines are normally distributed with a mean of zero and a standard deviation of 50 m, and the spatial decorrelation baseline is 1100 m. The revisiting time and radar wavelength, similar to Sentinel-1, are set to 12 days and 56 mm, respectively. The decorrelation rate is 200 days. The interferometric phases are only related to displacement with a velocity of 1 mm/year. The true data of interferometric phase matrix and coherence magnitude matrix are displayed in Figure 4a,b, respectively. Based on the complex coherence matrix, a stack of 40 images is simulated using a similar procedure to simulate polarimetric SAR images [60]. The size of the simulated image is 100 × 100 pixels. In addition, since the Γ ^ in Equation (15) is an average coherence, the S N R , B max , and B T max are empirically set to 12 dB, 1100 m and 200 days, respectively.
The values of s with a window of 5 × 5 and 7 × 7 pixels are shown in Figure 5, corresponding to the coherence matrix. From Figure 5a, it can be seen that s increases as the coherence magnitude decreases. Comparing Figure 5a,b, it can be found that s is larger when the sample number is smaller. These results are consistent with the theoretical analysis in Section 3.2, indicating the effectiveness of calculating s .
Figure 6 shows the results of coherence matrix estimation with a window of 5 × 5 pixels. Comparing the true data in Figure 4b and the sample coherence magnitude γ ^ in Figure 6a, overestimation can be clearly observed, and it is more severe over the low coherence interferogram. Correcting bias with the method proposed in [53], the coherence magnitude is improved to some extent. Nevertheless, overestimation can still be seen. By performing the correction method proposed in this paper, the coherence magnitude is significantly improved and asymptotically approaches the true data.
To further quantitative evaluation, the means and standard deviations of the estimated coherence magnitude are calculated from all N ( N 1 ) / 2 interferograms and all pixels, and shown in Figure 7. Considering that the pixel number of SHP set of a DS generally has a threshold [23], e.g., L > 20 , two windows with size of 5 × 5 and 7 × 7 pixels are set. From the means in Figure 7a, the overestimation by the sample coherence γ ^ can also be observed, and it is more severe when the number of looks is smaller. The mean bias is reduced by 64% by the correction coherence γ ¯ proposed in [53] over the sample coherence γ ^ . Compared with it, our proposed method achieves a significantly better correction with a bias reduction of more than 29% over the correction coherence γ ¯ . This is mainly because that s is appropriately assigned by considering the information on both interferometric coherence and the number of looks. In addition, comparing the standard deviations in Figure 7b, an average reduction of 33% by the corrected coherence γ ¯ over the sample coherence γ ^ , and 45% by the proposed coherence γ ˜ . The improvement of γ ˜ over γ ¯ is more than 18%. The lower biases and standard deviations indicate that the proposed method achieves more accurate coherence magnitude estimation. The qualitative and quantitative results jointly demonstrate the effectiveness of the proposed method in correcting the bias of coherence magnitude matrix, especially over the low coherence region.
The empirical standard deviation of phase residuals is calculated to provide the quantitative evaluation of phase optimization results. For i th image ( i 1 ), it is defined as
s t d i = 1 K j = 1 K ( R i , j R ¯ i ) 2
R i , j = arg ( exp ( j ( θ ^ i , j θ i , j ) ) )
where K is the total number of pixels of the simulated data. R i , j is the residual of the i th image and j th pixel. θ ^ i , j and θ i , j are the reconstructed phase and the truth value. arg ( ) denotes the argument of a complex number. R ¯ i is the mean residual of the i th image and can be estimated as 1 K j = 1 K R i , j . The smaller s t d means that the reconstructed phase is closer to the truth data.
To evaluate the improvement of coherence magnitude bias correction on phase optimization, different coherence magnitude matrices are used based on the EMI algorithm, and the corresponding standard deviations of residuals are displayed in Figure 8. The theoretically highest achievable precision is provided by the Cramér–Rao lower bound (CRLB) [32]. In general, for different methods, the precision of the phase optimization is higher when the number of looks is larger. This is because more samples can obtain a more accurate complex coherence matrix, including more accurate coherence magnitudes and interferometric phases. Comparing the results with different coherence, it can be found that the coherence magnitude has a noticeable influence on the accuracy of phase optimization. The reconstructed phase with coherence magnitude γ ˜ proposed in this paper has a higher precision than that with coherence magnitude γ ¯ and approaches the result with true coherence magnitude γ . The average phase residual with γ ˜ is 0.11 rad lower than that with γ ¯ . In addition, the reconstructed phases with γ ˜ have a higher precision, an average residual reduction of 0.48 rad, than traditional sample coherence magnitude γ ^ . This is equivalent to 2.4 mm deviations for the C-band of Sentinel-1, which can lead to a noticeable difference in deformation results. The simulation results demonstrate the effectiveness of performing coherence magnitude bias correction for phase optimization and the superiority of the proposed coherence bias correction method over the existing correction method in phase optimization.
The reconstructed phase series can be further evaluated by the multi-looking results of a single point. Figure 9 shows the results at any point and the true data. It can also be seen that the reconstructed phases from more samples are closer to the true data. In addition, the reconstructed phases with γ ˜ have slightly higher precision than that with γ ¯ and are significantly more accurate than that with γ ^ . The results further demonstrate that the proposed approach can obtain more accurate reconstructed phase series.

4.2. Test on Real InSAR Data Stacks

A stack of 40 Sentinel-1 images over the Volcán Alcedo is used to test the performance of the proposed algorithm. Figure 10 shows the optical and averaged SAR intensity data, revealing the variety of land cover in the scene. Sentinel-1 images are obtained in wide-swath mode and VV polarization, and from January 2021 to May 2022 in a descending orbit. The test region is limited to an area of 650 × 2400 pixels. The CMP algorithm is exploited to select SHPs in a 7 × 13 path. Only pixels with more than 20 SHPs are selected as DS candidates for phase estimation.
The performance of the proposed approach is visually assessed by inspecting the reconstructed interferograms with the longest temporal baseline of 288 days. The results are displayed in Figure 11. To better compare the details, a selected caldera indicated by the red rectangle is enlarged. A comparison of Figure 11a,b reveals a significant noise suppression of traditional EMI phase optimization. By adopting the corrected coherence magnitude γ ¯ , the results are improved with smoother interferometric phases. However, some noise points can still be clearly observed in Figure 11c. The result using the corrected coherence magnitude γ ˜ proposed in this paper is displayed in Figure 11d, which yields better reconstructed phases with fewer noise points..
The reconstructed interferograms can be further visualized by profile analyses. Figure 12 presents the profiles of original and reconstructed interferograms along the horizontal and vertical black solid lines depicted in Figure 11a. We can see that the profile lines from the corrected coherence magnitude γ ¯ are smoother than those from the sample coherence magnitude γ ^ , but still contain some outliers. Evidently, the proposed approach with the corrected coherence magnitude γ ˜ generates smoother profiles with fewer outliers. The better performance indicates the effectiveness of the proposed approach, and can be attributed to the effective correction of coherence magnitude bias.
Furthermore, a quantitative evaluation of the reconstructed phases is provided by the temporal coherence, which reads as [23]
γ P T A = 2 N ( N 1 ) i = 1 N j = i + 1 N cos ( φ ^ i , j θ ^ i + θ ^ j )
where φ ^ i , j is the interferometric phase in the coherence matrix T ^ . θ ^ i and θ ^ j are the reconstructed phase with the phase estimation algorithm. Figure 13 shows the histogram of temporal coherence for phase estimation using different coherence magnitude estimators. Improvements can be clearly found between the corrected coherence magnitude γ ¯ and the sample coherence magnitude γ ^ over the low temporal coherence regions ( γ P T A < 0.2 ), where the frequency is reduced to near zero by γ ¯ . The low temporal coherence regions ( 0.2 < γ P T A < 0.45 ) are further improved by the corrected coherence magnitude γ ˜ proposed in this paper. Visual inspection reveals that these improvements are mainly located in densely vegetated areas with low coherence magnitude, which corresponds to high coherence magnitude bias. The experimental results over real SAR data indicate the proposed phase estimation approach can reconstruct better phase series, including smoother phases, fewer outliers and higher temporal coherence.

5. Discussion

The current phase optimization algorithms, such as MLE [23,31], EVD [28,29], EMI [34] and NLEFIM [36], adopt the coherence matrix and its variant as the weight matrix [35]. Thus, the proposed coherence bias correction may be effective for all these phase optimization algorithms. The standard deviation of residuals with the sample coherence magnitude γ ^ and bias-corrected coherence magnitude γ ˜ are displayed in Figure 14. The simulated data in Section 4.1 is adopted and the size of SHP set is 7 × 7 pixels. It is clear that the corrected coherence magnitude obtains higher accuracy than the traditional sample coherence magnitude. The mean phase residuals are reduced by 0.32 rad, indicating the effectiveness and necessity of performing coherence bias correction. The accuracy improvements of MLE and EVD are more evident than those of EVD and NLEFIM. This is because that the inversion of coherence matrix is executed by the MLE and EMI, which amplify the coherence magnitude bias. When the sample coherence magnitude γ ^ is adopted, the NLEFIM is recommended to emphasize estimation accuracy. Since the power of EVD lies in separating scattering mechanisms from different heights, its accuracy is inferior to other methods. For MLE and EMI, the optimum performance can be achieved theoretically when their assumptions are valid. One of the violations of the assumptions is the coherence bias. Thus, the highest accuracy is obtained by MLE and EMI when the bias-corrected coherence magnitude is adopted. Considering that EMI has a computational efficiency advantage over MLE, our proposed phase estimation approach adopts the EMI algorithm.
To evaluate the computational efficiency, the processing time, including coherence matrix estimation and phase optimization, is provided in Figure 15 over the real data in Section 4.2. The image size is 650 × 2400 pixels and the search window size is 7 × 13 pixels. The calculation is in MATLAB R2019a software with an Intel Core I7 processor (3.0 GHz) and 32-GB RAM. In coherence matrix estimation procedure, Since the coherence bias correctors contain the processing of sample coherence estimation, the computational burden increases. The developed corrector is more complex due to the consideration of more information, and takes 2.5 times as long as the previous corrector. During the phase optimization procedure, computation with sample coherence estimation is time consuming. Compared with it, the processing time is improved by 42.2% by that with the previous correction, and by 43.1% by that with the proposed correction. This is because that the additional computation, regarding the coherence matrix regularization, is reduced. Fewer DSs with the non-positive definite coherence matrix are obtained by the developed correction. Considering the total processing time of the proposed approach is high, it is generally recommended for small-sized scenes. In addition, a possible strategy for large-sized images is to introduce high-performance parallel computing technology.

6. Conclusions

In this article, a modified DS phase estimation has been proposed for InSAR data stacks. The main contribution lies in effectively correcting the bias of coherence magnitude matrix. The core idea is to incorporate the information on both interferometric coherence and the number of looks to adaptively correct each element of the coherence matrix. The proposed approach is established by combing the coherence magnitude bias corrector, the CMP SHP selection and the EMI phase optimization, achieving high-precision phase reconstruction.
The experimental results with the simulated data have shown that more accurate coherence magnitude can be obtained by the proposed correction method, including lower mean bias (reduced by more than 29%) and smaller standard deviation (reduced by more than 18%), than the existing bias correction method. The reconstructed phase series with the proposed approach is closest to the CRLB, demonstrating the effectiveness of the results. The experimental results with the Sentinel-1 images also verify the effectiveness of the proposed approach with smoother interferometric phases and fewer outliers.

Author Contributions

Conceptualization, C.Z.; methodology, C.Z. and B.T.; software, C.Z.; validation, C.Z., J.Z. and Y.D.; formal analysis, C.Z. and W.W.; data curation, S.G., Y.Y. and L.H.; writing-original draft preparation, C.Z.; writing-review and editing, B.T., P.Z. and C.Z.; visualizations, C.Z.; supervision, Y.D.; project administration, W.W. and C.Z; funding acquisition, C.Z. and W.W. All authors have contributed significantly and have participated sufficiently to take responsibility for this research. All authors have read and agreed to the published version of the manuscript.

Funding

This work was supported by the Natural Science Basic Research Plan in Shaanxi Province of China under Grant 2022JQ-239, the National Natural Science Foundation of China under Grant 42004006 and 42071084, and the Fundamental Research Funds for the Central Universities under Grant GK202103130.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The data are contained within this article.

Acknowledgments

The author would like to thank the anonymous reviewers for the constructive as well as encouraging comments on this paper. The Sentinel-1 data were provided by the European Space Agency/Copernicus.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. (a) The difference between the expectation of sample coherence magnitude and true coherence γ for different numbers of looks L . (b) The standard deviation of sample coherence magnitude D ( γ ^ ) for different numbers of looks L .
Figure 1. (a) The difference between the expectation of sample coherence magnitude and true coherence γ for different numbers of looks L . (b) The standard deviation of sample coherence magnitude D ( γ ^ ) for different numbers of looks L .
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Figure 2. The difference between the estimated coherence magnitude γ ˜ and true coherence magnitude γ for different numbers of looks L and parameters s , using numerical calculation.
Figure 2. The difference between the estimated coherence magnitude γ ˜ and true coherence magnitude γ for different numbers of looks L and parameters s , using numerical calculation.
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Figure 3. Flowchart of the proposed phase estimation algorithm.
Figure 3. Flowchart of the proposed phase estimation algorithm.
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Figure 4. True data of (a) interferometric phase matrix and (b) coherence magnitude matrix.
Figure 4. True data of (a) interferometric phase matrix and (b) coherence magnitude matrix.
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Figure 5. The value of s with a window of (a) 5 × 5 pixels and (b) 7 × 7 pixels.
Figure 5. The value of s with a window of (a) 5 × 5 pixels and (b) 7 × 7 pixels.
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Figure 6. Coherence matrix estimation with a window of 5 × 5 pixels. (a) Sample coherence magnitude γ ^ . (b) Corrected coherence magnitude γ ¯ . (c) Corrected coherence magnitude γ ˜ with the proposed method.
Figure 6. Coherence matrix estimation with a window of 5 × 5 pixels. (a) Sample coherence magnitude γ ^ . (b) Corrected coherence magnitude γ ¯ . (c) Corrected coherence magnitude γ ˜ with the proposed method.
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Figure 7. (a) Means and (b) standard deviations for different coherence magnitude estimators using different numbers of looks.
Figure 7. (a) Means and (b) standard deviations for different coherence magnitude estimators using different numbers of looks.
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Figure 8. Standard deviation of the residuals for reconstructed phase series using different coherence magnitude estimators. The colors indicate the number of looks.
Figure 8. Standard deviation of the residuals for reconstructed phase series using different coherence magnitude estimators. The colors indicate the number of looks.
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Figure 9. Reconstructed phase series of a single point using different coherence magnitude estimators. The colors indicate the number of looks.
Figure 9. Reconstructed phase series of a single point using different coherence magnitude estimators. The colors indicate the number of looks.
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Figure 10. Study area in Volcán Alcedo. (a) Optical image from Google Earth. (b) Averaged intensity map from 40 SLCs of the Sentinel-1 image stacks.
Figure 10. Study area in Volcán Alcedo. (a) Optical image from Google Earth. (b) Averaged intensity map from 40 SLCs of the Sentinel-1 image stacks.
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Figure 11. The original and reconstructed interferometric phases with the longest temporal baseline of 288 days. An area denoted by the red rectangle is enlarged. (a) Original single look interferogram. Reconstructed phases using: (b) the sample coherence magnitude γ ^ , (c) the corrected coherence magnitude γ ¯ , (d) the corrected coherence magnitude γ ˜ proposed in this paper.
Figure 11. The original and reconstructed interferometric phases with the longest temporal baseline of 288 days. An area denoted by the red rectangle is enlarged. (a) Original single look interferogram. Reconstructed phases using: (b) the sample coherence magnitude γ ^ , (c) the corrected coherence magnitude γ ¯ , (d) the corrected coherence magnitude γ ˜ proposed in this paper.
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Figure 12. (a) Horizontal and (b) vertical profiles of original and reconstructed interferometric phases along solid black lines depicted in Figure 11a.
Figure 12. (a) Horizontal and (b) vertical profiles of original and reconstructed interferometric phases along solid black lines depicted in Figure 11a.
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Figure 13. Histogram of temporal coherence for phase estimation using different coherence magnitude estimators.
Figure 13. Histogram of temporal coherence for phase estimation using different coherence magnitude estimators.
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Figure 14. Standard deviation of the residuals for reconstructed phase series using different phase estimators. The colors indicate the coherence matrix estimator used.
Figure 14. Standard deviation of the residuals for reconstructed phase series using different phase estimators. The colors indicate the coherence matrix estimator used.
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Figure 15. Processing time over: (a) the coherence matrix estimation; (b) the EMI phase optimization.
Figure 15. Processing time over: (a) the coherence matrix estimation; (b) the EMI phase optimization.
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MDPI and ACS Style

Zhao, C.; Dong, Y.; Wu, W.; Tian, B.; Zhou, J.; Zhang, P.; Gao, S.; Yu, Y.; Huang, L. A Modification to Phase Estimation for Distributed Scatterers in InSAR Data Stacks. Remote Sens. 2023, 15, 613. https://doi.org/10.3390/rs15030613

AMA Style

Zhao C, Dong Y, Wu W, Tian B, Zhou J, Zhang P, Gao S, Yu Y, Huang L. A Modification to Phase Estimation for Distributed Scatterers in InSAR Data Stacks. Remote Sensing. 2023; 15(3):613. https://doi.org/10.3390/rs15030613

Chicago/Turabian Style

Zhao, Changjun, Yunyun Dong, Wenhao Wu, Bangsen Tian, Jianmin Zhou, Ping Zhang, Shuo Gao, Yuechi Yu, and Lei Huang. 2023. "A Modification to Phase Estimation for Distributed Scatterers in InSAR Data Stacks" Remote Sensing 15, no. 3: 613. https://doi.org/10.3390/rs15030613

APA Style

Zhao, C., Dong, Y., Wu, W., Tian, B., Zhou, J., Zhang, P., Gao, S., Yu, Y., & Huang, L. (2023). A Modification to Phase Estimation for Distributed Scatterers in InSAR Data Stacks. Remote Sensing, 15(3), 613. https://doi.org/10.3390/rs15030613

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