Volcanic eruptions in high resolution

高分辨率的火山喷发

• 批准号: 2102069
• 负责人: Emily Brodsky
• 金额: $ 33.99万
• 依托单位: University of California-Santa Cruz
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-08-01 至 2025-07-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2102069&HistoricalAwards=false
• 关键词: Volcanic; eruptions; resolution

Volcano seismology has focused on the times before and after eruptions. Although the most important part of a volcano’s lifecycle is the eruption itself, few earthquakes have been measured during the large, explosive phase of an eruption. This lack is because of the technical difficulties of measuring earthquakes while the eruption is producing a wide range of seismic noise. Here the researchers address this problem by using modern techniques of earthquake detection to chronicle the seismicity during a large-scale, explosive eruption. They illustrate the new approach with a preliminary analysis of the 2008 eruption of Mount Okmok; the volcano caldera, which exploded without warning, is located in the eastern Aleutian Islands of Alaska. Multiple techniques increase the number of detected events by factor of 4. Event rate varies in a non-trivial way during the eruption which cause is still unclear. Earthquakes appear to be recording a history of stress and failure that is related to, but distinct from the history of explosions. To better constrain earthquake rate during the eruption, the team re-analyzes recorded data using cutting-edge software. The trained algorithm is capable of identifying new seismic events among the noise. The new event catalog is used to better understand the volcano subterranean plumbing system. The same approach is applied to other volcanos in the Aleutians, Iceland, and Russia, which exhibit similar large eruptions. The comparative study allows evaluating whether volcano seismicity can be used to constrain subterranean magma cycle during large eruptions. The project provides support and training for one graduate student and undergraduate students, notably from underrepresented groups in science. Its outcomes improve volcanic hazard assessment, helping mitigating risks for local population and air traffic. The researchers propose to improve the co-eruptive seismic record of Okmok by utilizing an unsupervised, globally trained detection algorithm. The relationship between earthquake rate and the eruption cycle is still unclear. Not only is there an obvious increase in the earthquake rate at the eruption initiation, but there also appears to be a seismicity burst at the end of the eruption. Seismicity increases in the middle of the eruption may be associated with eruption reorganization but is not clearly associated with major plume-forming events. This may be a result of earthquakes’ sensitivity to the stresses in the solid crust rather than the eruptive processes in the conduit. Using the new record, the researchers identify and determine consistent magnitudes for the earthquakes. The new earthquakes at known magnitudes allow a self-consistent measure of earthquake rate throughout the eruption. It can be used to evaluate whether the earthquakes are marking the least open, most pressurized times and places. In the project second phase, the same methods are applied to other similarly large eruptions that have sufficient, publicly available seismic data. Those eruptions are: Grimsvotn, Kasatochi and Sheveluch. The team intends to explore the dataset of Nabro with an undergraduate, although it is not quite comparable. These comparative studies improve assessing the utility of earthquakes as an indicator of opened or closed volcano state. The expected outcomes will help understanding whether rapid fluctuations between pressurization and opening are common in major explosive eruptions.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

火山地震学关注的是火山爆发前后的时间。虽然火山生命周期中最重要的部分是喷发本身，但在喷发的大爆发阶段，很少有地震被测量到。这是因为测量地震的技术困难，而火山喷发会产生大范围的地震噪声。在这里，研究人员通过使用现代地震探测技术来记录大规模爆炸性喷发期间的地震活动来解决这个问题。他们通过对2008年玉木火山喷发的初步分析说明了这种新方法；位于阿拉斯加州阿留申群岛东部的火山口在没有任何预警的情况下爆发。多种技术将检测到的事件数量增加了4倍。在火山喷发期间，事件发生率发生了不小的变化，其原因尚不清楚。地震似乎记录了压力和失败的历史，这与爆炸的历史有关，但又不同。为了更好地控制火山喷发期间的地震频率，研究小组使用先进的软件重新分析了记录的数据。训练后的算法能够在噪声中识别新的地震事件。新的事件目录用于更好地了解火山地下管道系统。同样的方法也适用于阿留申群岛、冰岛和俄罗斯的其他火山，它们也表现出类似的大规模喷发。对比研究可以评估火山地震活动性是否可以用来约束大喷发期间的地下岩浆循环。该项目为一名研究生和本科生，特别是来自科学界代表性不足群体的学生提供支持和培训。其结果改进了火山灾害评估，有助于减轻当地居民和空中交通的风险。研究人员建议利用一种无监督的、全球训练的检测算法来改善Okmok的共喷发地震记录。地震频率与火山喷发周期之间的关系尚不清楚。不仅在喷发开始时地震率明显增加，而且在喷发结束时似乎也有一次地震活动爆发。火山喷发中期的地震活动性增加可能与火山喷发重组有关，但与主要火山柱形成事件的关系并不明显。这可能是由于地震对固体地壳中的应力敏感，而不是对管道中的喷发过程敏感。利用新的记录，研究人员确定并确定了地震的一致震级。已知震级的新地震可以在整个喷发过程中对地震率进行自我一致的测量。它可以用来评估地震是否标志着最不开放、压力最大的时间和地点。在项目的第二阶段，同样的方法被应用于其他类似的大型喷发，这些喷发有足够的、公开的地震数据。这些火山分别是：格里姆沃特火山、Kasatochi火山和舍韦鲁克火山。该团队打算与一名本科生一起探索Nabro的数据集，尽管它不太具有可比性。这些比较研究改进了地震作为火山开放或封闭状态指标的效用评估。预期的结果将有助于了解在压力和开放之间的快速波动是否在主要的爆炸性喷发中常见。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。

项目成果

A Specific Earthquake Processing Workflow for Studying Long‐Lived, Explosive Volcanic Eruptions With Application to the 2008 Okmok Volcano, Alaska, Eruption

用于研究长寿命、爆炸性火山喷发的特定地震处理工作流程并应用于 2008 年阿拉斯加奥克莫克火山喷发

• DOI: 10.1029/2022jb025882
• 发表时间: 2023
• 期刊: Journal of Geophysical Research: Solid Earth
• 作者: Garza‐Girón, Ricardo;Brodsky, Emily E.;Spica, Zack J.;Haney, Matthew M.;Webley, Peter W.
• 通讯作者: Webley, Peter W.

Earthquakes Record Cycles of Opening and Closing in the Enhanced Seismic Catalog of the 2008 Okmok Volcano, Alaska, Eruption

2008 年阿拉斯加奥克莫克火山喷发的增强地震目录中的地震记录了开闭周期

• DOI: 10.1029/2023jb026893
• 发表时间: 2023
• 期刊: Journal of Geophysical Research: Solid Earth
• 作者: Garza‐Girón, Ricardo;Brodsky, Emily E.;Spica, Zack J.;Haney, Matthew M.;Webley, Peter W.
• 通讯作者: Webley, Peter W.