Abstract

The characteristics of an earthquake can be derived by estimating the source geometries of the earthquake using parameter inversion that minimizes the L2 norm of residuals between the measured and the synthetic displacement calculated from a dislocation model. Estimating source geometries in a dislocation model has been regarded as solving a nonlinear inverse problem. To avoid local minima and describe uncertainties, the Monte-Carlo restarts are often used to solve the problem, assuming the initial parameter search space provided by seismological studies. Since search space size significantly affects the accuracy and execution time of this procedure, faulty initial search space from seismological studies may adversely affect the accuracy of the results and the computation time. Besides, many source parameters describing physical faults lead to bad data visualization. In this paper, we propose a new machine learning-based search space reduction algorithm to overcome these challenges. This paper assumes a rectangular dislocation model, i.e., the Okada model, to calculate the surface deformation mathematically. As for the geodetic measurement of three-dimensional (3D) surface deformation, we used the stacking interferometric synthetic aperture radar (InSAR) and the multiple-aperture SAR interferometry (MAI). We define a wide initial search space and perform the Monte-Carlo restarts to collect the data points with root-mean-square error (RMSE) between measured and modeled displacement. Then, the principal component analysis (PCA) and thek-means clustering are used to project data points with low RMSE in the 2D latent space preserving the variance of original data as much as possible and extractkclusters of data with similar locations and RMSE to each other. Finally, we reduce the parameter search space using the cluster with the lowest mean RMSE. The evaluation results illustrate that our approach achieves 55.1~98.1% reductions in search space size and 60~80.5% reductions in 95% confidence interval size for all source parameters compared with the conventional method. It was also observed that the reduced search space significantly saves the computational burden of solving the nonlinear least square problem.

Highlights

  • In the past decades, interferometric synthetic aperture radar (InSAR) has been a powerful method to acquire geophysical features such as surface deformation or topography by comparing the phases of at least two complex-valued SAR images obtained from different location or time

  • The evaluation was performed in terms of the size of search space, root-mean-square error (RMSE) calculated from determined source parameters, a 95% confidence interval of each source parameter, and the average iteration number of a nonlinear least square

  • The evaluation was performed in terms of the size of search space, RMSE values derived from determined source parameters, a 95% confidence interval of each source parameter, and the number of iterations for each nonlinear least square of the Monte-Carlo restarts

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Summary

Introduction

Interferometric synthetic aperture radar (InSAR) has been a powerful method to acquire geophysical features such as surface deformation or topography by comparing the phases of at least two complex-valued SAR images obtained from different location or time. Since SAR provides high-resolution images, InSAR can measure the surface deformation with centimetric or even millimetric accuracy. This accurate deformation map enables the observation of ocean and ground surface changes, the measurement of ice drift and glacier elevations, and the analysis of seismic deformation or volcanic activities [1]. Surface deformation acquired from InSAR measurements provides essential information for studying earthquakes and volcanic activities. The root-mean-square error (RMSE) values of residuals are used for the evaluation of the inversion result

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