From: Rapid emergency assessment of ash and gas hazard for future eruptions at Santorini Volcano, Greece
Model input parameter | Value | Description |
---|---|---|
Vent elevation | 113Â m | From Pyle and Elliot, 2006 |
Exit temperature | 1000Â K | Typical temperature of magmatic gases from dacitic magma |
Proportion of SO2 | 5Â % | As a proportion of erupted gas, the other gas being water |
Gas exit velocity | 10Â m/s | Estimate made from typical values |
Gas exit density | 0.12Â kg/m3 | Density of water at 1000Â K |
Vent diameter | 7 or 14Â m | Given gas density and concentration, a 7Â m diameter vent is required to emit 200 tons/day. To conserve mass, keeping temperature and velocity constant, an 800 tons/day emission requires a 14Â m diameter |
Albedo | 0.25 | Fraction of total incident solar radiation reflected by the surface (typical value for grassland used) |
Bowen ratio | 5 | Net radiation at a surface (typical value for grassland used) |
Surface roughness | 0.15Â m | Typical value for grassland used |