日本地球惑星科学連合2018年大会

講演情報

[JJ] 口頭発表

セッション記号 S (固体地球科学) » S-VC 火山学

[S-VC40] 火山防災の基礎と応用

2018年5月24日(木) 15:30 〜 17:00 A04 (東京ベイ幕張ホール)

コンビーナ:吉本 充宏(山梨県富士山科学研究所)、宝田 晋治(産業技術総合研究所活断層・火山研究部門)、石峯 康浩(鹿児島大学地域防災教育研究センター、共同)、久保 智弘(防災科学技術研究所)、座長:石峯 康浩(鹿児島大学地域防災教育研究センター)、宝田 晋治(産総研地質調査総合センター)、吉本 充宏(山梨県富士山科学研究所)

16:45 〜 17:00

[SVC40-12] Statistical Analysis of the Distribution of Ballistic Deposits using the BALLISTA Model

*常松 佳恵1ケネディー ベン2クリストファー ゴメス3フィッツジェラルド レベッカ2ショパール バスチャン4 (1.山梨県富士山科学研究所、2.カンタベリー大学地質学科、3.神戸大学大学院海事科学研究科、4.ジュネーブ大学コンピューターサイエンス学科)

キーワード:火山岩塊/噴石、確率論的手法、数値シミュレーション、バリスタ、ハウスドルフ距離

We present a statistical analysis of an inversion model using BALLISTA. BALLISTA is a program for simulating ballistic trajectories and ground deposition with many particles in 3D. It is a forward model, which means that it simulates the particles being ejected from the vent and falling on the ground. However, in many cases, we need to estimate the ejection conditions based on the information of particles on the ground. Therefore, it is necessary to create an inversion model.

We need to compare the distributions of the observed particles and the simulated particles, and then quantitively assess the difference between them. The Hausdorff distance is applied for this evaluation. The Hausdorff distance is often used in image analysis and is a mathematical construct to measure the "closeness" of two sets of points that are subsets of a metric space. The distributions of observed and simulated particles were represented by the convex hull which is drawn by Grass GIS without subjective discrimination, and their Hausdorff distance is calculated. Each simulation results in different distributions because the BALLISTA model is stochastic. Therefore, we investigated the value change of the Hausdorff distances by varying the drag coefficient, ejection velocity and investigate the variation caused by the stochastic nature of rerunning the same simulation. This analysis is applied to the ground distribution of ballistic projectiles from the Tongariro 2012 eruption which is documented by Fitzgerald et al. (2014). We discuss the ejection conditions obtained for the Tongariro case, and how many simulations are necessary for reaching the convergence of the Hausdorff distance.