A review of laboratory and numerical modelling in volcanology

Modelling has been used in the study of volcanic systems for more than 100 years, building upon the approach first applied by Sir James Hall in 1815. Informed by observations of volcanological phenomena in nature, including eye-witness accounts of eruptions, geophysical or geodetic monitoring of...

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Main Authors: J. L. Kavanagh, S. L. Engwell, S. A. Martin
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:Solid Earth
Online Access:https://www.solid-earth.net/9/531/2018/se-9-531-2018.pdf
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spelling doaj-9e582658aa0a44f3813b8f065cb57d202020-11-24T21:54:06ZengCopernicus PublicationsSolid Earth1869-95101869-95292018-04-01953157110.5194/se-9-531-2018A review of laboratory and numerical modelling in volcanologyJ. L. Kavanagh0S. L. Engwell1S. A. Martin2Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 3GP, UKBritish Geological Survey, The Lyell Centre, Research Avenue South, Edinburgh EH14 4AP, UKDepartment of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool L69 3GP, UKModelling has been used in the study of volcanic systems for more than 100 years, building upon the approach first applied by Sir James Hall in 1815. Informed by observations of volcanological phenomena in nature, including eye-witness accounts of eruptions, geophysical or geodetic monitoring of active volcanoes, and geological analysis of ancient deposits, laboratory and numerical models have been used to describe and quantify volcanic and magmatic processes that span orders of magnitudes of time and space. We review the use of laboratory and numerical modelling in volcanological research, focussing on sub-surface and eruptive processes including the accretion and evolution of magma chambers, the propagation of sheet intrusions, the development of volcanic flows (lava flows, pyroclastic density currents, and lahars), volcanic plume formation, and ash dispersal. <br><br> When first introduced into volcanology, laboratory experiments and numerical simulations marked a transition in approach from broadly qualitative to increasingly quantitative research. These methods are now widely used in volcanology to describe the physical and chemical behaviours that govern volcanic and magmatic systems. Creating simplified models of highly dynamical systems enables volcanologists to simulate and potentially predict the nature and impact of future eruptions. These tools have provided significant insights into many aspects of the volcanic plumbing system and eruptive processes. The largest scientific advances in volcanology have come from a multidisciplinary approach, applying developments in diverse fields such as engineering and computer science to study magmatic and volcanic phenomena. A global effort in the integration of laboratory and numerical volcano modelling is now required to tackle key problems in volcanology and points towards the importance of benchmarking exercises and the need for protocols to be developed so that models are routinely tested against <q>real world</q> data.https://www.solid-earth.net/9/531/2018/se-9-531-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. L. Kavanagh
S. L. Engwell
S. A. Martin
spellingShingle J. L. Kavanagh
S. L. Engwell
S. A. Martin
A review of laboratory and numerical modelling in volcanology
Solid Earth
author_facet J. L. Kavanagh
S. L. Engwell
S. A. Martin
author_sort J. L. Kavanagh
title A review of laboratory and numerical modelling in volcanology
title_short A review of laboratory and numerical modelling in volcanology
title_full A review of laboratory and numerical modelling in volcanology
title_fullStr A review of laboratory and numerical modelling in volcanology
title_full_unstemmed A review of laboratory and numerical modelling in volcanology
title_sort review of laboratory and numerical modelling in volcanology
publisher Copernicus Publications
series Solid Earth
issn 1869-9510
1869-9529
publishDate 2018-04-01
description Modelling has been used in the study of volcanic systems for more than 100 years, building upon the approach first applied by Sir James Hall in 1815. Informed by observations of volcanological phenomena in nature, including eye-witness accounts of eruptions, geophysical or geodetic monitoring of active volcanoes, and geological analysis of ancient deposits, laboratory and numerical models have been used to describe and quantify volcanic and magmatic processes that span orders of magnitudes of time and space. We review the use of laboratory and numerical modelling in volcanological research, focussing on sub-surface and eruptive processes including the accretion and evolution of magma chambers, the propagation of sheet intrusions, the development of volcanic flows (lava flows, pyroclastic density currents, and lahars), volcanic plume formation, and ash dispersal. <br><br> When first introduced into volcanology, laboratory experiments and numerical simulations marked a transition in approach from broadly qualitative to increasingly quantitative research. These methods are now widely used in volcanology to describe the physical and chemical behaviours that govern volcanic and magmatic systems. Creating simplified models of highly dynamical systems enables volcanologists to simulate and potentially predict the nature and impact of future eruptions. These tools have provided significant insights into many aspects of the volcanic plumbing system and eruptive processes. The largest scientific advances in volcanology have come from a multidisciplinary approach, applying developments in diverse fields such as engineering and computer science to study magmatic and volcanic phenomena. A global effort in the integration of laboratory and numerical volcano modelling is now required to tackle key problems in volcanology and points towards the importance of benchmarking exercises and the need for protocols to be developed so that models are routinely tested against <q>real world</q> data.
url https://www.solid-earth.net/9/531/2018/se-9-531-2018.pdf
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