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RiskScape has a modular structure, with hazard layers, assets, and loss functions prepared separately.
The effect of directionality or topography is ignored for simplicity: it is likely the hazard layers overestimate hazard intensity and resulting damage.
Future work should include incorporating uncertainty in the vulnerability models and the hazard layers in order to allow quantification of the uncertainty in the loss estimates.
We briefly describe how the hazard layers for the edifice, pyroclastic surge, tephra fall, and lava were generated; for more detail refer to Deligne et al. (2017).
Hazard layers may be input in any coordinate system (the user must specify which one) and for anywhere in the world.
Deligne et al. (2017) used the nearby prehistoric AVF Maungataketake eruption (~85 89 ka) as an analogue AVF eruption when developing hazard layers due to similar substrates and relative sea level (Agustín-Flores et al., 2014).
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The hazard layer is input in raster format, with the raster provided by the user.
Seventeen urban areas, main highways, large lakes, and a greyscale digital elevation model underlie the transparent hazard layer as background features.
As it is not based on lava flow modelling, the hazard layer ignores effects of lava flow/water interactions, lava flow rheology, and finer scale topographic influences.
Two methods have previously been employed and include the use of GIS hazard layer (e.g. geology, topography) analysis or airborne electromagnetic (EM) mapping.
The hazard layer is input in raster format, either from a user-provided raster or one generated through on-the-fly modelling within the RiskScape programme.
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