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Constraining Tephra Aggregation Efficiency with Laboratory Experiments and Numerical Modeling

Constraining Tephra Aggregation Efficiency with Laboratory Experiments and Numerical Modeling
通过实验室实验和数值模拟约束 Tephra 聚集效率
批准号:
1249999
负责人:
Leah Courtland
金额:
$8.5万
依托单位:
依托单位国家:
美国
项目类别:
Fellowship Award
财政年份:
2013
资助国家:
美国
项目状态:
已结题
起止时间:
2013-06-01 至 2015-05-31

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中文摘要
翻译
Leah Courtland博士被授予美国国家科学基金会地球科学博士后奖学金,在佐治亚理工学院开展一项研究和教育计划。这项研究将使用实验室实验和数值模拟相结合的方法,更好地限制火山灰在火山羽流最上方区域的聚集速度。实验室实验将利用冰核室来对不同相对湿度和外加电场强度下的Tephra聚集速率进行参数化。主要目的是提高我们对大气中的火山灰对火山羽流中普遍存在的相对湿度条件以及这些羽流中存在电场的反应的了解。实验的结果将是不同羽流条件(湿度、温度、电场)下颗粒尺寸分布的预期变化的参数化。如果成功,这将允许Tephra弥散模型使用近实时的气象数据来更好地预测颗粒在大气中的停留时间。研究结果将有助于限制危机应对情景中使用的Tephra危险模型。这些模型的改进最终将导致提高航空安全和更有效地减轻地面远场火山灰撞击的灾害战略。Tephra尘埃是火山喷发最深远的危险,能够导致屋顶坍塌、污染供水、破坏关键设施,并威胁人和牲畜的健康。2010年,冰岛埃亚菲亚德拉火山喷发,向大气层喷发了几天的火山灰,实际上关闭了欧洲大部分空域,影响了数十万旅客,给航空业造成了数十亿美元的损失。这一事件的全球性和严重的经济后果表明,迫切需要准确地预测大气和地面上的火山灰分布情况。虽然过去40年来对火山灰的输送和沉积的研究极大地增加了我们对这些过程的理解,并使数值模型的开发能够模拟火山灰的扩散,但当代的火山灰模型还没有以有意义的方式捕捉到大量细小的火山灰(63um)注入大气中。模型计算和火山喷发的真实分布之间的差异反映了大多数模型未能考虑到自然过程,这些自然过程将火山喷发出的细灰作为更大集合体的组成部分迅速从大气中移除。为了促进对火山灰聚集的了解,同时培养大学生的榜样素养和量化技能,将通过Vhub.org网络平台设计和实施一系列教育模块。VHub.org是一个火山建模和教育的在线资源。这项工作产生的火山灰聚集的数值参数最终也将安装在Vhub.org上,以方便更大的科学界使用该模型。
英文摘要
Dr. Leah Courtland has been awarded an NSF Earth Science Postdoctoral Fellowship to carry out a research and education plan at Georgia Institute of Technology. This study will use a combination of laboratory experiments and numerical modeling to better constrain the rate of tephra (volcanic ash) aggregation in the uppermost regions of volcanic plumes. Laboratory experiments will utilize an ice nucleation chamber to parameterize the rate of tephra aggregation under a variety of relative humidities and applied electric field strengths. The main goal is to improve our understanding of the response of tephra in the atmosphere to the relative humidity conditions prevalent in volcanic plumes and the presence of an electric field within these plumes. The result of experiments will be a parameterization of the expected change in particle size distribution for varying plume conditions (humidity, temperature, electrical field). If successful, this will allow tephra dispersion models to use near-real- time meteorological data to better forecast particle residence time in the atmosphere. Research results will help to constrain tephra hazard models used in crisis response scenarios. Improvement in these models should ultimately lead to increased aviation safety and more effective hazard mitigation strategies for far-field tephra impacts on the ground.Tephra fallout is the most far reaching hazard of volcanic eruptions, capable of causing roof collapse, polluting water supplies, damaging critical facilities, and threatening the health of people and livestock. The 2010 eruption of Eyjafjallajökull in Iceland spewed ash into the atmosphere for days, effectively shutting down most of European air space, affecting hundreds of thousands of travelers, and costing the aviation industry billions of dollars. The global nature and high economic consequence of this event expose an urgent need for accurate forecasts of the distribution of tephra in the atmosphere and on the ground. While the study of the transport and sedimentation of volcanic ash over the last forty years has greatly increased our understanding of these processes and enabled the development of numerical models to simulate tephra dispersion, the injection of large volumes of fine (63 um) ash into the atmosphere is not yet captured in a meaningful way by the current generation of tephra models. The discrepancy between model calculations and the true distribution of tephra reflects the failure of the majority of models to account for natural processes that rapidly remove the fine ash fraction of volcanic ejecta from the atmosphere as constituent pieces of larger aggregates. To facilitate understanding of ash aggregation while fostering model literacy and quantitative skills building among university students, a series of educational modules will be designed and implemented via the Vhub.org web platform. VHub.org is an online resource for volcano modeling and education. The numerical parameterization of ash aggregation to result from this work will ultimately be installed on Vhub.org as well, in order facilitate use of the model by the larger scientific community.
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