Abstract
The idea of this special issue comes out from a discussion at the workshop Uncertainty Quantification in Lava Flow Hazard Modeling and Real-Time Source Term Provision held in Istituto Nazionale di Geofisica e Vulcanologia (INGV) in Catania (Italy) during Febraury 2017.
Highlights
The idea of this special issue comes out of discussions at the workshop on “Uncertainty Quantification in Lava Flow Hazard Modeling and Real-Time Source Term Provision” held at the Istituto Nazionale di Geofisica e Vulcanologia (INGV) in Catania (Italy) during February 2017
The results suggest that the MIR-derived radiant flux essentially mimics the overall trend of lava discharge rates, with only a minor influence due to the emplacement style and evolving eruptive conditions
The results show that incorporating a two-component emissivity model linked to the fraction of molten lava and cooled crust is an important factor for model accuracy and is especially critical for large, high effusion rate flows
Summary
MONITORING THE TIME-AVERAGED DISCHARGE RATES, VOLUMES AND EMPLACEMENT STYLE OF LARGE LAVA FLOWS BY.
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