4.3 Article

Results of the eruptive column model inter-comparison study

期刊

出版社

ELSEVIER
DOI: 10.1016/j.jvolgeores.2016.01.017

关键词

Explosive volcanism; Eruptive plumes dynamics; Fluid dynamic models; Model inter-comparison; Eruption source parameters

资金

  1. International Research Promotion Office Earthquake Research Institute, the University of Tokyo
  2. EU [308665, 308,377]
  3. NSF Postdoctoral Fellowship [EAR1250029]
  4. USGS Mendenhall Fellowship
  5. NSF-IDR
  6. AFOSR
  7. NERC [NE/I01554X/1]
  8. INSU, CNRS
  9. NERC [NE/I01554X/1] Funding Source: UKRI
  10. Natural Environment Research Council [NE/I01554X/1] Funding Source: researchfish
  11. Grants-in-Aid for Scientific Research [25750142] Funding Source: KAKEN
  12. Directorate For Engineering
  13. Div Of Civil, Mechanical, & Manufact Inn [1131074] Funding Source: National Science Foundation
  14. Division Of Earth Sciences
  15. Directorate For Geosciences [1250029] Funding Source: National Science Foundation

向作者/读者索取更多资源

This study compares and evaluates one-dimensional (1D) and three-dimensional (3D) numerical models of volcanic eruption columns in a set of different inter-comparison exercises. The exercises were designed as a blind test in which a set of common input parameters was given for two reference eruptions, representing a strong and a weak eruption column under different meteorological conditions. Comparing the results of the different models allows us to evaluate their capabilities and target areas for future improvement. Despite their different formulations, the 1D and 3D models provide reasonably consistent predictions of some of the key global descriptors of the volcanic plumes. Variability in plume height, estimated from the standard deviation of model predictions, is within similar to 20% for the weak plume and similar to 10% for the strong plume. Predictions of neutral buoyancy level are also in reasonably good agreement among the different models, with a standard deviation ranging from 9 to 19% (the latter for the weak plume in a windy atmosphere). Overall, these discrepancies are in the range of observational uncertainty of column height. However, there are important differences amongst models in terms of local properties along the plume axis, particularly for the strong plume. Our analysis suggests that the simplified treatment of entrainment in 1D models is adequate to resolve the general behaviour of the weak plume. However, it is inadequate to capture complex features of the strong plume, such as large vortices, partial column collapse, or gravitational fountaining that strongly enhance entrainment in the lower atmosphere. We conclude that there is a need to more accurately quantify entrainment rates, improve the representation of plume radius, and incorporate the effects of column instability in future versions of 1D volcanic plume models. (C) 2016 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.3
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据