ABR: Toward Seismic Tomography Based Upon Adjoint Methods

ABR：基于伴随方法的地震层析成像

• 批准号: 1112906
• 负责人: Jeroen Tromp
• 金额: $ 71万
• 依托单位: Princeton University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-07-01 至 2016-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1112906&HistoricalAwards=false
• 关键词: ABR; Toward; Seismic; Tomography; Based

The primary goal of this project is to use seismic data to image Earth structure and seismic sources based on modern numerical methods and imaging techniques. We will further develop and enhance software for the simulation of 3D seismic wave propagation, with a particular emphasis on computing on Graphics Processing Units, rather than traditional Central Processing Units, potentially providing an order of magnitude increase in simulation speed. The broader impacts of the proposal include open-source software packages for the simulation of seismic wave propagation. Simulations based on these packages may be used to investigate seismic hazard and aid in the determination of tomographic images of Earth's interior and earthquake source parameters. All software developed during the course of the proposed research period will be made freely available via the Computational Infrastructure for Geodynamics (geodynamics.org).The simulations of seismic wave propagation account for heterogeneity in Earth's crust and mantle, topography& bathymetry, seismic anisotropy, attenuation, fluid-solid interactions, self-gravitation, rotation, and the oceans. The main intellectual merit of this project revolves around harnessing the power of the forward modeling tools to enhance the quality of images of Earth's interior and the earthquake rupture process. The approach is to minimize remaining between simulated and observed seismograms based on so-called adjoint techniques in combination with conjugate gradient methods, an approach we refer to as "adjoint tomography". Specifically, following a successful application in southern California, we will 1) develop open-source GPU-based forward and adjoint spectral-element solvers, 2) perform adjoint tomography of Europe, 3) further develop noise cross-correlation tomography based on adjoint methods, 4) move towards adjoint tomography of the entire planet, and 5) extend the southern California and global "ShakeMovie" cyber infrastructure.

该项目的主要目标是根据现代数值方法和成像技术，利用地震数据对地球结构和震源进行成像。我们将进一步开发和增强三维地震波传播模拟软件，特别强调图形处理单元而不是传统的中央处理单元的计算，从而可能使模拟速度提高一个数量级。该提案的更广泛影响包括用于模拟地震波传播的开放源码软件包。基于这些软件包的模拟可用于调查地震危险性，并有助于确定地球内部和震源参数的层析成像图像。在拟议的研究期间开发的所有软件将通过地球动力学计算基础设施（geodynamics.org）免费提供。地震波传播模拟考虑了地壳和地幔的不均匀性、地形测深、地震各向异性、衰减、流体-固体相互作用、自引力、旋转和海洋。该项目的主要智力价值围绕着利用正演建模工具的力量来提高地球内部和地震破裂过程图像的质量。该方法是最大限度地减少剩余的模拟和观测地震图的基础上，结合共轭梯度法，我们称之为“伴随层析成像”的方法，所谓的伴随技术。具体而言，在南加州成功应用后，我们将1）开发基于GPU的开源前向和伴随谱元解算器，2）执行欧洲的伴随层析成像，3）进一步开发基于伴随方法的噪声互相关层析成像，4）迈向整个地球的伴随层析成像，以及5）扩展南加州和全球“ShakeMovie”网络基础设施。