volcanological scenario (typified by mass of erupted magma, the plume height, the
dimension of tephra, duration of the event) was chosen and simulated by using a large data
set
of meteorological conditions. For Hekla the scenario is the1980 eruption, for Katla it is the
1918 eruption and for Öræfajökull it is the 1362 eruption. Input parameters for the dispersal
model have been defined in order
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf