A parametric and comparative study of different tephra fallout models
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| Title: | A parametric and comparative study of different tephra fallout models |
|---|---|
| Authors: | Scollo, S.1 scollo@ct.ingv.it, Folch, A.2, Costa, A.2 |
| Source: | Journal of Volcanology & Geothermal Research. Sep2008, Vol. 176 Issue 2, p199-211. 13p. |
| Subjects: | Volcanic ash, tuff, etc., Volcanic eruptions, Particles, Fragmentation reactions |
| Abstract: | Abstract: We perform a parametric and comparative study on three different tephra dispersal models (FALL3D, HAZMAP, and TEPHRA) applied to two different scenarios expected for Etna volcano. These scenarios are similar to the recent 2002–03 and 1990 Etna eruptions and correspond, respectively, to a weak and to a strong plume eruption. For each model and scenario we perform a parametric study on several inputs in order to quantify how a variation on a given input parameter (i.e. an uncertainty on the model input) affects the results of the model. The study considers topographic effects, different description for the eruption column, column height influence, different fits for terminal velocities of particles, the effect of particle shape and, finally, the variation of the modal grain-size. Model differences are quantified by means of a normalized distance that indicates how close, in average, the results from two different simulations are. We also compare predictions from different models to determine under which circumstances the use of a more elaborated model is justified. Results from our parametric study show that output of the models can be strongly sensitive to the uncertainties and assumptions on input parameters, such as mainly mass eruption rate, column height, distribution of the mass along the column, bulk grain-size distribution. This highlights that, for optimal forecasts, is urgent to improve the description of these parameters and of some important physical processes like fragmentation and eruption column dynamics. Further, differences between models are often lower than those due to the uncertainties of input parameters, although they become more high in simulating weak plumes. Thus the choice of the model mainly depends on the kind of application such as the need to simulate the evolution of volcanic clouds in the atmosphere. Finally, the use of both a semi-analytical (HAZMAP) and a fully computational (FALL3D) model for inverting field data of the 2001 Etna eruption showed that the best-fit parameters are similar for both models, and are consistent with values obtained using independent techniques. [Copyright &y& Elsevier] |
| Copyright of Journal of Volcanology & Geothermal Research is the property of Elsevier B.V. and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | Engineering Source |
| FullText | Text: Availability: 0 |
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| Header | DbId: egs DbLabel: Engineering Source An: 34439298 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: A parametric and comparative study of different tephra fallout models – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Scollo%2C+S%2E%22">Scollo, S.</searchLink><relatesTo>1</relatesTo><i> scollo@ct.ingv.it</i><br /><searchLink fieldCode="AR" term="%22Folch%2C+A%2E%22">Folch, A.</searchLink><relatesTo>2</relatesTo><br /><searchLink fieldCode="AR" term="%22Costa%2C+A%2E%22">Costa, A.</searchLink><relatesTo>2</relatesTo> – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+Volcanology+%26+Geothermal+Research%22">Journal of Volcanology & Geothermal Research</searchLink>. Sep2008, Vol. 176 Issue 2, p199-211. 13p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Volcanic+ash%2C+tuff%2C+etc%2E%22">Volcanic ash, tuff, etc.</searchLink><br /><searchLink fieldCode="DE" term="%22Volcanic+eruptions%22">Volcanic eruptions</searchLink><br /><searchLink fieldCode="DE" term="%22Particles%22">Particles</searchLink><br /><searchLink fieldCode="DE" term="%22Fragmentation+reactions%22">Fragmentation reactions</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Abstract: We perform a parametric and comparative study on three different tephra dispersal models (FALL3D, HAZMAP, and TEPHRA) applied to two different scenarios expected for Etna volcano. These scenarios are similar to the recent 2002–03 and 1990 Etna eruptions and correspond, respectively, to a weak and to a strong plume eruption. For each model and scenario we perform a parametric study on several inputs in order to quantify how a variation on a given input parameter (i.e. an uncertainty on the model input) affects the results of the model. The study considers topographic effects, different description for the eruption column, column height influence, different fits for terminal velocities of particles, the effect of particle shape and, finally, the variation of the modal grain-size. Model differences are quantified by means of a normalized distance that indicates how close, in average, the results from two different simulations are. We also compare predictions from different models to determine under which circumstances the use of a more elaborated model is justified. Results from our parametric study show that output of the models can be strongly sensitive to the uncertainties and assumptions on input parameters, such as mainly mass eruption rate, column height, distribution of the mass along the column, bulk grain-size distribution. This highlights that, for optimal forecasts, is urgent to improve the description of these parameters and of some important physical processes like fragmentation and eruption column dynamics. Further, differences between models are often lower than those due to the uncertainties of input parameters, although they become more high in simulating weak plumes. Thus the choice of the model mainly depends on the kind of application such as the need to simulate the evolution of volcanic clouds in the atmosphere. Finally, the use of both a semi-analytical (HAZMAP) and a fully computational (FALL3D) model for inverting field data of the 2001 Etna eruption showed that the best-fit parameters are similar for both models, and are consistent with values obtained using independent techniques. [Copyright &y& Elsevier] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Journal of Volcanology & Geothermal Research is the property of Elsevier B.V. and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
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| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1016/j.jvolgeores.2008.04.002 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 13 StartPage: 199 Subjects: – SubjectFull: Volcanic ash, tuff, etc. Type: general – SubjectFull: Volcanic eruptions Type: general – SubjectFull: Particles Type: general – SubjectFull: Fragmentation reactions Type: general Titles: – TitleFull: A parametric and comparative study of different tephra fallout models Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Scollo, S. – PersonEntity: Name: NameFull: Folch, A. – PersonEntity: Name: NameFull: Costa, A. IsPartOfRelationships: – BibEntity: Dates: – D: 20 M: 09 Text: Sep2008 Type: published Y: 2008 Identifiers: – Type: issn-print Value: 03770273 Numbering: – Type: volume Value: 176 – Type: issue Value: 2 Titles: – TitleFull: Journal of Volcanology & Geothermal Research Type: main |
| ResultId | 1 |
