CAREER: Subduction Zone Hazards: Megathrust Rupture Dynamics and Tsunamis

职业：俯冲带危险：巨型逆冲断层破裂动力学和海啸

• 批准号: 1255439
• 负责人: Eric Dunham
• 金额: $ 56.94万
• 依托单位: Stanford University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2013
• 资助国家: 美国
• 起止时间: 2013-07-01 至 2018-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1255439&HistoricalAwards=false
• 关键词: CAREER; Subduction; Zone; Hazards; Megathrust

Subduction zones are home to two of the most spectacular and dangerous natural hazards on Earth: megathrust earthquakes and tsunamis. To mitigate risk, we must better understand the earthquake cycle in subduction zones: What fraction of relative plate motion is accommodated aseismically instead of seismically, and to what extent do estimates of the seismic coupling coefficient allow one to predict the extent of future megathrust earthquakes? What role does inelastic deformation of the accretionary prism play in rupture dynamics? What determines the up-dip extent of slip, a key factor controlling the seafloor uplift and tsunami height? And what causes the slow rupture process of tsunami earthquakes that produce vastly larger tsunamis than expected from the amplitude of seismic waves at periods less than ~10 s? These questions will be addressed with three-dimensional numerical simulations capable of resolving interseismic loading, creep and slow slip, and fully dynamic spontaneous ruptures, with realistic geometries and heterogeneous material structure. The solid Earth component of the model will be fully coupled to a compressible ocean, in order to simultaneously capture seismic waves, hydroacoustic (ocean sound) waves, and surface gravity waves (tsunamis). Attention will be placed on the hydroacoustic signature of subduction earthquakes, as recorded by ocean bottom pressure sensors. Hydroacoustic waves excited by seafloor displacement arrive at the coast many minutes before the tsunami, and could potentially be used to estimate tsunami wave heights for use in early warning systems. Simulations will be conducted for the 2011 Tohoku-Oki earthquake and other recent events, and comparisons made to seismic, geodetic, tsunami, and ocean acoustic data. The largest earthquakes on Earth occur in subduction zones along the boundary between tectonic plates, such as the Cascadia subduction zone offshore Washington and Oregon. These earthquakes cause vertical uplift of the seafloor, generating tsunamis. This project is aimed at characterizing hazards from these earthquakes and tsunamis using computational simulations coupling the response of the solid Earth, including frictional sliding along faults, and the ocean. The simulations will capture the earthquake rupture process, as well as excitation and propagation of seismic waves, hydroacoustic waves (sound waves in the ocean), and tsunamis.Specific models will be developed for the 2011 Tohoku-Oki, Japan, earthquake and other recent events, and comparison made to a range of geophysical data to validate the modeling approach. Preliminary simulations of the Tohoku-Oki earthquake suggest that hydroacoustic waves, which can be recorded by cabled ocean bottom pressure sensors deployed tens or a hundred kilometers offshore, might be used to rapidly estimate tsunami wave heights for use in an early warning system. This research effort will be complemented with an outreach education program aimed an increasing awareness of and preparedness for natural hazards in the Central Coast region of California, through a partnership between Stanford and Allan Hancock College (AHC), a Hispanic-serving community college in the Central Coast. The PI will work with faculty and students at AHC to develop earthquake and tsunami demonstrations and activities for use in AHC?s Friday Night Science outreach programs attended by 600?1000 members of the community. Each summer, the PI will host an AHC student in an eight-week research internship at Stanford.

俯冲带是地球上两种最壮观和最危险的自然灾害的所在地：大推力地震和海啸。为了降低风险，我们必须更好地了解俯冲带的地震周期：相对板块运动的哪一部分是抗震性的而不是地震性的，地震耦合系数的估计在多大程度上允许人们预测未来巨型逆冲断层地震的程度？增生棱柱的非弹性变形在破裂动力学中扮演什么角色？是什么决定了滑动的上倾程度，这是控制海底隆起和海啸高度的关键因素？是什么导致了海啸地震的缓慢破裂过程，产生了比预期的更大的海啸，从地震波的振幅在小于10秒的周期？这些问题将通过三维数值模拟来解决，这些模拟能够解决地震间载荷、蠕变和缓慢滑动以及完全动态的自发破裂，具有逼真的几何形状和异质材料结构。该模型的固体地球部分将完全耦合到可压缩的海洋，以便同时捕获地震波，水声（海洋声波）波和表面重力波（海啸）。将注意海底压力传感器记录的俯冲地震的水声特征。海底位移激发的水声波在海啸发生前几分钟到达海岸，可能用于估计海啸波高，以供预警系统使用。将对2011年东北冲岐地震和其他近期事件进行模拟，并与地震、大地测量、海啸和海洋声学数据进行比较。 地球上最大的地震发生在构造板块之间边界的沿着俯冲带，例如华盛顿和俄勒冈州近海的卡斯卡迪亚俯冲带。这些地震导致海底垂直隆起，产生海啸。该项目的目的是利用计算模拟，将固体地球的反应，包括沿沿着的摩擦滑动和海洋的反应结合起来，描述这些地震和海啸的危害。模拟将捕捉地震破裂过程，以及地震波、水声波（海洋中的声波）和海啸的激发和传播。将为2011年日本东北冲地震和其他近期事件开发特定模型，并与一系列地球物理数据进行比较，以验证建模方法。对东北冲地震的初步模拟表明，可以通过部署在离岸数十或一百公里处的海底电缆压力传感器记录的水声波，可以用于快速估计海啸波高，以用于早期预警系统。这项研究工作将补充一个外展教育计划，旨在提高认识和防备自然灾害在加州的中央海岸地区，通过斯坦福大学和艾伦汉考克学院（AHC），在中央海岸的西班牙裔服务社区学院之间的伙伴关系。PI将与AHC的教师和学生合作，开发用于AHC的地震和海啸演示和活动。星期五晚上的科学推广计划有600人参加？社区的1000名成员。每年夏天，PI将在斯坦福大学举办为期八周的研究实习AHC学生。