CAREER: Integrating earthquake physics and source imaging while engaging the Hispanic community

职业：整合地震物理和震源成像，同时吸引西班牙裔社区

• 批准号: 1151926
• 负责人: Jean-Paul Ampuero
• 金额: $ 56.3万
• 依托单位: California Institute of Technology
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-06-15 至 2018-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1151926&HistoricalAwards=false
• 关键词: CAREER; Integrating; earthquake; physics; source

The main research goal of this project is to understand the origin of earthquake rupture complexity and its impact on destructive ground motions by narrowing the gap between theoretical and computational earthquake dynamics and observational earthquake source seismology, while significantly advancing both. This research integrates theory and observations to enhance the capacity to extract reliable constraints on earthquake rupture processes from seismological data. It provides a computational environment to address open questions and formulate testable hypothesis about the physics of earthquakes. The proposed developments in computational seismology tackle the multi-scale aspects of earthquake dynamics by consolidating two methods that can handle realistic geometries and rheologies, the spectral element method (SEM) and the discontinuous Galerkin method, by applying space-time adaptive techniques to dynamic rupture problems and by extending the SEM simulation capabilities to the longer time-scales of the earthquake cycle. The proposed observational developments introduce multi-scale signal analysis concepts in source imaging techniques based on back-projection of high-frequency seismic array data and integrate these results with more traditional source inversion approaches at lower frequencies. The 2011 M9 Tohoku (Japan) mega-earthquake is a main focus of the integrative efforts. Synergistic activities between theory and observations characterize the uncertainties in source imaging through realistic synthetic scenarios and mitigate those uncertainties by integrating adequate prior information in the source inversion problem. The education and outreach activities of this project engage the Hispanic community in enhancing its scientific literacy about earthquake processes, to reduce its vulnerability to seismic hazards. This is achieved by regular workshops for the Hispanic media, by engaging Hispanic undergraduate summer interns, by assessing in collaboration with social scientists the cultural factors of vulnerability in the Hispanic population, by developing school activities that link earthquake hazards and Hispanic heritage and by involving Latinos of Southern California in low-cost seismic networks. In addition, software products and related training materials are made openly available and the research results are integrated in graduate teaching.This research addresses an outstanding challenge in earthquake science: resolving and interpreting the multi-scale complexity of dynamic rupture. The project integrates two distinct directions of earthquake research, theoretical/computational earthquake physics and observational seismology, through synergy between physics-based simulation and data-based earthquake rupture imaging. This research improves our general understanding of multi-scale processes in dynamic fracture and provides related software and analysis tools with potential applications in other disciplines, e.g. for the assessment of the reliability of heterogeneous engineering materials. The research products enhance the capacity of rapid response to mitigate the destructive effects of earthquakes globally. The project naturally involves international collaborations. The educational activities foster inter-disciplinary interactions between seismology and social science, and foster the participation in scientific education and research of an underrepresented group, the Hispanic community, while reducing its vulnerability to natural hazards

该项目的主要研究目标是通过缩小理论和计算地震动力学与观测震源地震学之间的差距，了解地震破裂复杂性的起源及其对破坏性地震动的影响，同时显著推进两者的发展。本研究将理论与观测相结合，以提高从地震资料中提取地震破裂过程可靠约束的能力。它提供了一个计算环境来解决开放的问题和制定可测试的假设关于地震的物理。计算地震学的发展建议通过整合两种可以处理实际几何和流变的方法，即谱元方法（SEM）和不连续Galerkin方法，通过将时空自适应技术应用于动态破裂问题，并通过将SEM模拟能力扩展到地震周期的更长时间尺度，来解决地震动力学的多尺度方面。提出的观测发展在基于高频地震阵列数据反投影的震源成像技术中引入了多尺度信号分析概念，并将这些结果与更传统的低频震源反演方法相结合。2011年日本东北9级大地震是综合工作的主要焦点。理论和观测之间的协同活动通过现实的综合场景表征了源成像的不确定性，并通过在源反演问题中集成足够的先验信息来减轻这些不确定性。该项目的教育和外联活动使西班牙裔社区参与提高其对地震过程的科学素养，以减少其对地震灾害的脆弱性。通过定期为西班牙裔媒体举办研讨会，通过让西班牙裔本科生暑期实习生参与进来，通过与社会科学家合作评估西班牙裔人口中易受伤害的文化因素，通过开展将地震灾害与西班牙裔遗产联系起来的学校活动，以及通过让南加州的拉丁裔人参与低成本地震网络来实现这一目标。此外，软件产品和相关培训资料公开，并将研究成果融入研究生教学。本研究解决了地震科学中的一个突出挑战：解决和解释动态破裂的多尺度复杂性。该项目整合了两个不同的地震研究方向，即理论/计算地震物理学和观测地震学，通过物理模拟和基于数据的地震破裂成像之间的协同作用。这项研究提高了我们对动态断裂多尺度过程的总体理解，并提供了相关的软件和分析工具，在其他学科中具有潜在的应用前景，例如异质工程材料的可靠性评估。研究成果提高了快速反应能力，以减轻全球地震的破坏性影响。该项目自然涉及国际合作。这些教育活动促进了地震学和社会科学之间的跨学科互动，并促进了西班牙裔社区这一代表性不足的群体参与科学教育和研究，同时减少了其对自然灾害的脆弱性