Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan

Vulcanian eruptions (short-lived explosions consisting of a rising thermal) occur daily in volcanoes around the world. Such small-scale eruptions represent a challenge in numerical modeling due to local-scale effects, such as the volcano’s topography impact on atmospheric circulation and near-vent p...

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Main Authors: Kosei Takishita, Alexandros P. Poulidis, Masato Iguchi
Format: Article
Language:English
Published: MDPI AG 2021-03-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/3/331
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author Kosei Takishita
Alexandros P. Poulidis
Masato Iguchi
author_facet Kosei Takishita
Alexandros P. Poulidis
Masato Iguchi
author_sort Kosei Takishita
collection DOAJ
description Vulcanian eruptions (short-lived explosions consisting of a rising thermal) occur daily in volcanoes around the world. Such small-scale eruptions represent a challenge in numerical modeling due to local-scale effects, such as the volcano’s topography impact on atmospheric circulation and near-vent plume dynamics, that need to be accounted for. In an effort to improve the applicability of Tephra2, a commonly-used advection-diffusion model, in the case of vulcanian eruptions, a number of key modifications were carried out: (i) the ability to solve the equations over bending plume, (ii) temporally-evolving three-dimensional meteorological fields, (iii) the replacement of the particle diameter distribution with observed particle terminal velocity distribution which provides a simple way to account for the settling velocity variation due to particle shape and density. We verified the advantage of our modified model (Tephra4D) in the tephra dispersion from vulcanian eruptions by comparing the calculations and disdrometer observations of tephra sedimentation from four eruptions at Sakurajima volcano, Japan. The simulations of the eruptions show that Tephra4D is useful for eruptions in which small-scale movement contributes significantly to ash transport mainly due to the consideration for orographic winds in advection.
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spelling doaj.art-e3e7cb5bf60847619ea7e8101c2edd692023-12-03T12:31:23ZengMDPI AGAtmosphere2073-44332021-03-0112333110.3390/atmos12030331Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, JapanKosei Takishita0Alexandros P. Poulidis1Masato Iguchi2Sakurajima Volcano Research Center, DPRI, Kyoto University, Kagoshima 841-1419, JapanSakurajima Volcano Research Center, DPRI, Kyoto University, Kagoshima 841-1419, JapanSakurajima Volcano Research Center, DPRI, Kyoto University, Kagoshima 841-1419, JapanVulcanian eruptions (short-lived explosions consisting of a rising thermal) occur daily in volcanoes around the world. Such small-scale eruptions represent a challenge in numerical modeling due to local-scale effects, such as the volcano’s topography impact on atmospheric circulation and near-vent plume dynamics, that need to be accounted for. In an effort to improve the applicability of Tephra2, a commonly-used advection-diffusion model, in the case of vulcanian eruptions, a number of key modifications were carried out: (i) the ability to solve the equations over bending plume, (ii) temporally-evolving three-dimensional meteorological fields, (iii) the replacement of the particle diameter distribution with observed particle terminal velocity distribution which provides a simple way to account for the settling velocity variation due to particle shape and density. We verified the advantage of our modified model (Tephra4D) in the tephra dispersion from vulcanian eruptions by comparing the calculations and disdrometer observations of tephra sedimentation from four eruptions at Sakurajima volcano, Japan. The simulations of the eruptions show that Tephra4D is useful for eruptions in which small-scale movement contributes significantly to ash transport mainly due to the consideration for orographic winds in advection.https://www.mdpi.com/2073-4433/12/3/331tephraadvection-diffusion modeldisdrometerSakurajimaTephra2Tephra4D
spellingShingle Kosei Takishita
Alexandros P. Poulidis
Masato Iguchi
Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
Atmosphere
tephra
advection-diffusion model
disdrometer
Sakurajima
Tephra2
Tephra4D
title Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
title_full Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
title_fullStr Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
title_full_unstemmed Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
title_short Tephra4D: A Python-Based Model for High-Resolution Tephra Transport and Deposition Simulations—Applications at Sakurajima Volcano, Japan
title_sort tephra4d a python based model for high resolution tephra transport and deposition simulations applications at sakurajima volcano japan
topic tephra
advection-diffusion model
disdrometer
Sakurajima
Tephra2
Tephra4D
url https://www.mdpi.com/2073-4433/12/3/331
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