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The peak value of velocity provides the input for a numerical model of plume rise.
Wet deposition is based on a model of plume scavenging by the rain.
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The model simulation of plume transportation was relatively easy in this early phase during which there was no precipitation.
The estimated eruption velocities serve as the input for numerical models of plume rise.
The high emissions, complex topography, wind circulation, and its closeness to MCMA have prompted the monitoring and modeling of plume dispersion from the Miguel Hidalgo Oil Refinery and the Francisco Perez Rios Power Plant and their effects on the northern sector of the MCMA.
The realism of the plume model simulations was tested by comparing model calculations of plume concentrations with data of SF6 tracer concentrations and ozone concentrations.
Therefore, in a PTS event with pronounced plume cooling a detailed model of the plume has to be considered in the structural analysis.
To date, we have applied this model regardless of plume size; however, the Working Group on Advanced VAFF (2013b) suggested that this approach might not be accurate for small eruptions.
Quantitative proof for DOC degradation under iron-reducing conditions could only be obtained if the geochemical processes cation exchange and precipitation of carbonate minerals (siderite and calcite) were considered and incorporated in an inverse geochemical model of the plume.
We demonstrate history matching on an integral model of volcanic plumes that is used to estimate source conditions from observations of the rise height of plumes during the eruptions of Eyjafjallajökull, Iceland, in 2010 and Grímsvötn, Iceland, in 2011.
An integral model of volcanic plumes is then introduced.
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