综合后滑数据伴随同化法估计摩擦参数和模拟变量初值

M. Kano, S. Miyazaki, Kosuke Ito, K. Hirahara
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引用次数: 5

摘要

由于板块边界滑动的变化取决于摩擦特性,因此了解断层上的摩擦参数以及模拟变量的初始值对于地震发生预测至关重要。在本研究中,将伴随数据同化方法引入到一个简单的模型中。以速率和状态相关的摩擦律建立故障模型,以实现在实际情况下估计摩擦参数和仿真变量初值的目标。该方法适用于简单体。该模型模拟了2003年的枥树余震。通过人为赋值“真”摩擦参数和初始值,合成了断层表面滑动速度数据集。在已知“背景”值和观测值的前提下,研究了用伴随数据同化方法估计摩擦参数和初始值的可行性。结果表明,与网格搜索法相比,伴随数据同化法通过对观测数据的时间轨迹拟合估计摩擦参数和初始值等控制变量具有较高的计算效率。此外,我们还研究了每个摩擦参数和初始值对观测到的后滑速度数据的敏感性。在我们使用后滑数据搜索的范围内,我们发现1)速度的初值可以被约束,2)状态变量的初值不能被约束,3)a-b的摩擦参数值在观测到后滑速度的区域可以很好地检索到,4)特征长度L的值只能从后滑速度数据的早期部分检索到,那里的速度变化很快。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of Frictional Parameters and Initial Values of Simulation Variables Using an Adjoint Data Assimilation Method with Synthetic Afterslip Data
Since variations of slip on plate boundaries depend on frictional properties, it is essential to know frictional parameters on the fault, as well as initial values of simulation variables for earthquake generation prediction. In this study, an adjoint data assimilation method is introduced to a simpli.ed fault model with a rate-and state-dependent friction law as a .rst step toward the goal of estimating the frictional parameters and initial values of simulation variables in a realistic situation. The method is applied to the simpli.ed model which mimics the 2003 Tokachi-oki afterslip. We make synthetic data set, slip velocities on the fault surface by assigning the “true” frictional parameters and initial values artificially. We investigate the feasibility of estimating frictional parameters and initial values through the adjoint data assimilation method on the assumption of knowing “background” values and observations. It is confirmed that the adjoint data assimilation method is computationally efficient to estimate control variables such as frictional parameters and initial values by time-trajectory fitting of observation data, compared to the grid search method. Also, we examine the sensitivity of each frictional parameter and initial value to the observed afterslip velocity data. In the range of our search using afterslip data, we .nd that 1) the initial value of velocity can be constrained, 2) the initial value of state variable cannot be constrained, 3) the frictional parameter value of a-b is well retrieved in the region where aftreslip velocity is observed, and 4) the value of characteristic length L can be retrieved only from the early portion of afterslip velocity data, where the velocity is rapidly changing.
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