Abstract

Atmospheric propagation delay correction is the key to improving the accuracy of deformation measurement of satellite interferometric synthetic aperture radar (InSAR). The empirical phase-elevation models and external data-based models present uneven performances of atmospheric delay correction for InSAR deformation monitoring. In this study, based on our previous fusion of delays predicted by multiple weather models (FDWM), we propose a new approach of adaptive fusion of multi-source tropospheric delay (AFMTD) estimates derived from multiple models over wide areas, i.e., ERA5, GACOS, WRF, MERRA2, NARR, MODIS, Linear model, and Powerlaw model. The spatially varying scaling algorithm is employed to refine the tropospheric delays predicted by the weather models. Meanwhile, we adopt a multiple-window strategy to cope with the spatially lateral variation of tropospheric delays. The AFMTD not only improves the spatial heterogeneity of tropospheric delay, but also adaptively combines multiple models to achieve a more reliable delay estimation. This AFMTD method is incorporated into the StaMPS-SBAS procedure. We compared the AFMTD with other single models using ENVISAT ASAR and Sentinel-1 datasets over Los Angeles of Southern California. The result of ASAR first demonstrates the effectiveness and reliability of the AFMTD method by referring to the assumed ground truth of simultaneous MERIS observations. The results of Sentinel-1 data show that over 95% of unwrapped interferograms have the minimum root-mean-square values after AFMTD correction for both descending and ascending tracks. The validation against GPS observation presents that the RMSEs of InSAR displacement time series after AFMTD correction decreases at more than 90% of 125 GPS stations. The average reductions of RMSE are 35.79% and 36.28% for descending and ascending data, respectively, and the maximum improvement is more than 70%. Overall, the proposed AFMTD method outperforms any single model for InSAR tropospheric delay correction and provides an open framework to fuse multi-source tropospheric delay estimates.

Highlights

  • The atmospheric propagation delay (APD), which stemmed from the refraction of electromagnetic waves when propagating in the nonhomogeneous atmosphere, is a major confusing source in interferometric synthetic aperture radar (InSAR) deformation measurements (Zebker et al, 1997)

  • The effectiveness of adaptive fusion of multi-source tropospheric delay (AFMTD) method was first evaluated on ENVISAT ASAR data using the integrated precipitable water vapor from MERIS

  • We analyzed the applicability of AFMTD method to correct tropospheric delays for frequently-used Sentinel-1 data, which is validated by the GPS measurements

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Summary

INTRODUCTION

The atmospheric propagation delay (APD), which stemmed from the refraction of electromagnetic waves when propagating in the nonhomogeneous atmosphere, is a major confusing source in InSAR deformation measurements (Zebker et al, 1997). The tropospheric delays depend on the variations in atmospheric parameters between SAR acquisitions. Dong et al (2019) proposed a fusion model named FDWM that combines tropospheric delays derived from multiple weather models to correct the stratified delay when monitoring single landslides. Shen et al (2019) proposed the spatially varying scaling (abbreviated as SVS here) algorithm to alleviate the deviation in the estimated tropospheric delay from its truth. Based on the framework of our previous FDWM fusion model (Dong et al, 2019), we propose a new method to adaptively fuse more tropospheric delays estimated or predicted by the empirical models (Linear and Powerlaw), meteorological reanalysis models (ERA5, GACOS, MERRA2, and NARR), numerical weather forecast model (WRF), and multi-spectral image (MODIS). The new method adopts the SVS algorithm to alleviate the deviation of tropospheric delays calculated by the external weather models. Track Pass Number of SAR images Number of interferograms Resolution (Az × Rg) Incidence angle Polarization Time span

64 Ascending
RESULTS AND ANALYSES
DISCUSSION
CONCLUSION
DATA AVAILABILITY STATEMENT
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