DS-InSAR phase optimization based on singular value decomposition

  • role: First author第一作者
  • Affiliation:

    School of Environment Science and Spatial Information, China University of Mining and Technology, Xuzhou 221116, China

    The Key Laboratory of Land Environment and Disaster Monitoring, MNR, China University of Mining and Technology,Xuzhou 221116, China

  • Email:1634612853@qq.com
  • Introduction:InSARE-mail 1634612853@qq.com
PENG Kai12,  
  • Affiliation:

    School of Environment Science and Spatial Information, China University of Mining and Technology, Xuzhou 221116, China

    The Key Laboratory of Land Environment and Disaster Monitoring, MNR, China University of Mining and Technology,Xuzhou 221116, China

ZHAO Feng12,  
  • role: Corresponding author通信作者
  • Affiliation:

    School of Environment Science and Spatial Information, China University of Mining and Technology, Xuzhou 221116, China

    The Key Laboratory of Land Environment and Disaster Monitoring, MNR, China University of Mining and Technology,Xuzhou 221116, China

  • Email:wyj4139@163.com
  • Introduction:E-mail wyj4139@163.com
WANG Yunjia12*,  
  • Affiliation:

    School of Environment Science and Spatial Information, China University of Mining and Technology, Xuzhou 221116, China

    The Key Laboratory of Land Environment and Disaster Monitoring, MNR, China University of Mining and Technology,Xuzhou 221116, China

YAN Shiyong12,  
  • Affiliation:

    School of Environment Science and Spatial Information, China University of Mining and Technology, Xuzhou 221116, China

    The Key Laboratory of Land Environment and Disaster Monitoring, MNR, China University of Mining and Technology,Xuzhou 221116, China

FENG Han12

реферат

The spatial density of high-quality monitoring points is an important indicator for time-series InSAR to carry out deformation monitoring. Relying on Distributed Scatterers (DS) to carry out InSAR deformation monitoring can effectively solve the defect of insufficient spatial density of traditional time-series InSAR monitoring points, but the interferometric phase of distributed scatterers is easily affected by decoherence, causing the interferometric phase distortion and unreliable, so the phase optimization of distributed scatterers is the key to DS-InSAR technology and is particularly significant. Aiming at this situation, this paper proposes a new DS phase optimization method based on singular value decomposition. This method reconstructs the phase matrix by using the time-series phase of homogeneous pixels, which belong to the same substance within the inspection window, and performs principal component analysis on the matrix to obtain the optimized phase. As a very necessary step, simulation data and 33 scene coverages of Sentinel-1A data in Baisha town, eastern Zhengzhou, are used to verify the reliability and validity of the proposed method. Using time-series average phase standard deviation, average phase gradient, and average number of residual points as the evaluation index of interferogram optimization effect, the index of the interferogram optimized by the proposed method is reduced by 15.61%, 25.81%, and 44.84% respectively compared with the original interferogram, which shows that these indicators have significant decreases. The results show that, compared with the contrast DS phase optimization method, the proposed method has a better effect on the interferogram DS phase optimization, especially in some areas with poor coherence and low signal to noise ratio. In addition, the proposed method can better maintain the detailed information of the ground features while reducing the DS phase noise. Besides, compared with the deformation monitoring results of the conventional PS(Permanent Scatterers)-InSAR technology, the number of high-quality monitoring points in this method has increased from 121471 to 644789, an increase of 4.3 times, and the density of high-quality monitoring points has increased more significantly than the comparison method. The experimental results of the simulation and real data confirm the effectiveness of the DS optimization method proposed in this paper, which can be used in DS-InSAR technology for surface deformation monitoring.

ключеви́че слова́

remote sensing;DS-InSAR;distributed scatterers;phase optimization;singular value decomposition;deformation monitoring

References

  1. 1.
    Cao N, Lee H and Jung H C. 2015. Mathematical framework for phase-triangulation algorithms in distributed-scatterer interferometry. IEEE Geoscience and Remote Sensing Letters, 12(9): 1838-1842
  2. 2.
    Cao N, Lee H and Jung H C. 2016. A phase-decomposition-based PSInSAR processing method. IEEE Transactions on Geoscience and Remote Sensing, 54(2): 1074-1090
  3. 3.
    Deledalle C A, Denis L and Tupin F. 2011. NL-InSAR: nonlocal interferogram estimation. IEEE Transactions on Geoscience and Remote Sensing, 49(4): 1441-1452
  4. 4.
    Ferretti A, Fumagalli A, Novali F, Prati C, Rocca F and Rucci A. 2011. A new algorithm for processing interferometric Data-Stacks: SqueeSAR. IEEE Transactions on Geoscience and Remote Sensing, 49(9): 3460-3470
  5. 5.
    Ferretti A, Prati C and Rocca F. 2001. Permanent scatterers in SAR interferometry. IEEE Transactions on Geoscience and Remote Sensing, 39(1): 8-20
  6. 6.
    Fornaro G, Verde S, Reale D and Pauciullo A. 2015. CAESAR: an approach based on covariance matrix decomposition to improve multibaseline-multitemporal interferometric SAR processing. IEEE Transactions on Geoscience and Remote Sensing, 53(4): 2050-2065
  7. 7.
    Goldstein R M and Werner C L. 1998. Radar interferogram filtering for geophysical applications. Geophysical Research Letters, 25(21): 4035-4038
  8. 8.
    Hooper A, Segall P and Zebker H. 2007. Persistent scatterer interferometric synthetic aperture radar for crustal deformation analysis, with application to Volcán Alcedo, Galápagos. Journal of Geophysical Research, 112(B7): B07407
  9. 9.
    Hooper A, Zebker H, Segall P and Kampes B. 2004. A new method for measuring deformation on volcanoes and other natural terrains using InSAR persistent scatterers. Geophysical Research Letters, 31(23): L23611
  10. 10.
    Hooper A and Zebker H A. 2007. Phase unwrapping in three dimensions with application to InSAR time series. Journal of the Optical Society of America A, 24(9): 2737-2747
  11. 11.
    Jiang M, Ding X L, Hanssen R F, Malhotra R and Chang L. 2015. Fast statistically homogeneous pixel selection for covariance matrix estimation for multitemporal InSAR. IEEE Transactions on Geoscience and Remote Sensing, 53(3): 1213-1224
  12. 12.
    Jiang M, Ding X L and Li Z W. 2014. Hybrid approach for unbiased coherence estimation for multitemporal InSAR. IEEE Transactions on Geoscience and Remote Sensing, 52(5): 2459-2473
  13. 13.
    Kalman D. 1996. A singularly valuable decomposition: the SVD of a matrix. The College Mathematics Journal, 27(1): 1-23
  14. 14.
    Lee J S, Cloude S R, Papathanassiou K P, Grunes M R and Woodhouse I H. 2003. Speckle filtering and coherence estimation of polarimetric SAR interferometry data for forest applications. IEEE Transactions on Geoscience and Remote Sensing, 41(10): 2254-2263
  15. 15.
    Li Z L, Zou W B, Ding X L, Chen Y Q and Liu G X. 2004. A quantitative measure for the quality of INSAR interferograms based on phase differences. Photogrammetric Engineering and Remote Sensing, 70(10): 1131-1137
  16. 16.
    Zhao F and Mallorqui J J. 2019. A temporal phase coherence estimation algorithm and its application on DInSAR pixel selection. IEEE Transactions on Geoscience and Remote Sensing, 57(11): 8350-8361
  17. 17.
    Jiang M, Ding X L and Li Z W. 2018. Homogeneous pixel selection algorithm for multitemporal InSAR. Chinese Journal of Geophysics, 61(12): 4767-4776
  18. 18.
    Zhu J J, Li Z W and Hu J. 2017. Research progress and methods of InSAR for deformation monitoring. Acta Geodaetica et Cartographica Sinica, 46(10): 1717-1733
  19. 19.
    Zhu J J, Yang Z F and Li Z W. 2019. Recent progress in retrieving and predicting mining-induced 3D displace-ments using InSAR. Acta Geodaetica et Cartographica Sinica, 48(2): 135-144

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