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PLUME-MoM-TSM 1.0.0: a volcanic column and umbrella cloud spreading model

机译:Plume-Mom-TSM 1.0.0:火山柱和伞云扩展模型

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In?this paper, we present a new version of PLUME-MoM, a 1-D integral volcanic plume model based on the method of moments for the description of the polydispersity in solid particles. The model describes the steady-state dynamics of a plume in a 3-D coordinate system, and a modification of the two-size moment (TSM) method is adopted to describe changes in grain size distribution along the plume, associated with particle loss from plume margins and with particle aggregation. For this reason, the new version is named PLUME-MoM-TSM. For the first time in a plume model, the full Smoluchowski coagulation equation is solved, allowing us to quantify the formation of aggregates during the rise of the plume. In addition, PLUME-MOM-TSM allows us to model the phase change of water, which can be either magmatic, added at the vent as liquid from external sources, or incorporated through ingestion of moist atmospheric air. Finally, the code includes the possibility to simulate the initial spreading of the umbrella cloud intruding from the volcanic column into the atmosphere. A transient shallow-water system of equations models the intrusive gravity current, allowing computation of the upwind spreading. The new model is applied first to the eruption of the Calbuco volcano in southern Chile in April 2015 and then to a sensitivity analysis of the upwind spreading of the umbrella cloud to mass flow rate and meteorological conditions (wind speed and humidity). This analysis provides an analytical relationship between the upwind spreading and some observable characteristic of the volcanic column (height of the neutral buoyancy level and plume bending), which can be used to better link plume models and volcanic-ash transport and dispersion models.
机译:在译文中,我们介绍了一种新的Plume-MOM,基于矩的矩的1-D整体火山羽模型,用于在固体颗粒中的多分散性描述。该模型描述了3-D坐标系中的羽流的稳态动态,采用两尺寸时刻(TSM)方法的修改来描述沿着羽毛的晶粒尺寸分布的变化,与粒子损失相关羽毛利润和颗粒聚集。因此,新版本名为Plume-Mom-TSM。首次在羽流模型中,解决了全斯莫氏露凝凝凝结构,允许我们在羽流升高期间量化聚集体的形成。此外,Plume-MOM-TSM允许我们模拟水的相变,可以是岩浆,从外部的液体添加到液体中,或者通过摄取湿气氛空气。最后,该代码包括模拟从火山柱侵入大气中的伞云的初始扩展的可能性。瞬态浅水系统的方程式模型侵入式重力电流,允许计算上风扩散。 2015年4月首先应用新型模型,首先应用于智利南部的Calbuco火山喷发,然后对伞云的逆风扩散到质量流量和气象条件(风速和湿度)进行敏感性分析。该分析提供了对火山柱的上风扩散和一些可观察特性之间的分析关系(中性浮力水平和羽流弯曲的高度),可用于更好地连接羽流模型和火山灰运输和分散模型。

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