Detecting, Modelling and Responding to Effusive Eruptions
CONTAINS OPEN ACCESS
For effusive volcanoes in resource-poor regions, there is a pressing need for a crisis response-chain bridging the global scientific community to allow provision of standard products for timely humanitarian response. As a first step in attaining this need, this Special Publication provides a complete directory of current operational capabilities for monitoring effusive eruptions. This volume also reviews the state-of-the-art in terms of satellite-based volcano hot-spot tracking and lava-flow simulation. These capabilities are demonstrated using case studies taken from well-known effusive events that have occurred worldwide over the last two decades at volcanoes such as Piton de la Fournaise, Etna, Stromboli and Kilauea. We also provide case-type response models implemented at the same volcanoes, as well as the results of a community-wide drill used to test a fully-integrated response focused on an operational hazard-GIS. Finally, the objectives and recommendations of the ‘Risk Evaluation, Detection and Simulation during Effusive Eruption Disasters’ working group are laid out in a statement of community needs by its members.
LavaSIM: its physical basis and applicability
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Published:January 01, 2016
Abstract
LavaSIM is a lava -flow simulator to carry out three-dimensional (3D) analysis of solid–liquid two-phase lava flows. Heat transfer between molten lava and solidified crust into the air, water and ground is calculated using radiation equations, so we can simulate not only the lava-flow distribution but also its physical characteristics: for instance, the internal convectional structure. Lava viscosity can be treated as a function of temperature, and is associated with the percentage of crystallization. The stop condition for the lava flow is determined by calculating the minimum spreading thickness, taking into consideration the yield strength. This paper also discusses whether LavaSIM, the deterministic lava-flow simulation, can be applied to basaltic lava flows and allow lava-flow characteristics, such as inundated area, temperature distribution, crust–melt distribution, velocity and pressure field, to be quantitatively evaluated.
- applications
- Asia
- basalt flows
- case studies
- crystallization
- dynamics
- effusion
- equations
- eruptions
- Europe
- Far East
- flow mechanism
- geologic hazards
- heat flow
- heat transfer
- Honshu
- Italy
- Izu-Oshima
- Izu-shichito
- Japan
- Kirishima
- Kyushu
- lava flows
- mathematical methods
- Mount Etna
- Mount Mihara
- natural hazards
- numerical models
- physical properties
- rheology
- Sicily Italy
- simulation
- Southern Europe
- temperature
- viscosity
- volcanism
- volcanoes
- yield strength
- Shinmoe-dake
- LavaSIM