4.7 Article

A Refined Strategy for Removing Composite Errors of SAR Interferogram

期刊

IEEE GEOSCIENCE AND REMOTE SENSING LETTERS
卷 11, 期 1, 页码 143-147

出版社

IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/LGRS.2013.2250903

关键词

Composite errors; elevation-dependent phase error; linear model; synthetic aperture radar interferometry (InSAR); quadratic model

资金

  1. National Natural Science Foundation of China [41222027, 40974006]
  2. National High-Tech. Research and Development Program of China [2012AA121301]
  3. National Key Basic Research and Development Program of China [2012CB719903]
  4. Research Grants Council of the Hong Kong Special Administrative Region [PolyU 5154/10E]

向作者/读者索取更多资源

In standard differential synthetic aperture radar interferometry, there could still be a residual tilt (orbital error) in the interferometric phase due to inaccurate baseline estimation. We demonstrated theoretically that the orbital errors were partially elevation dependent. On the basis of this, we introduced an elevation-dependent item to the conventional polynomial model to simulate, and therefore, compensate the orbital errors, as well as the small scale topographic and/or topography-related phase errors. Robust regression approach was suggested to determine the parameters of the proposed model. The model was validated with both synthetic and real ALOS PALSAR data of the Zhouqu, China mudslide. The synthetic test indicated that upon applying the refined model, the accuracies of phase measurements were improved by nearly two times, compared to those using conventional linear and quadratic models. The real data experiment indicated that after utilizing the refined model, the correlation between the interferogram and the digital elevation model of Zhouqu reduced to about 1/5 of those using linear and quadratic models. This demonstrates that the elevation-dependent phase components have been largely removed by the new model. More importantly, the interferogram corrected by the new model visibly disclosed the deformation area affected by the Zhouqu mudslide.

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