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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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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