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In positive pressure mode, the compressor is pressure source.
Upward changes represent extension by inflation of the pressure source.
First, we assumed a spherical pressure source (Fig. 2a).
Estimated location of the pressure sources beneath Sakurajima volcano.
a Modeled pressure source based on GEONET data alone.
b Modeled pressure sources based on GEONET and JMANET data.
The star is the location of the pressure source.
The parameters are the location of pressure source, time of pressure increase, and hydraulic diffusivity.
We examined two source types, a spherical pressure source and a tensile crack source.
For example, geodetic data analyses are useful for determining the locations and sizes of volcanic pressure sources by applying pressure source models (Mogi, 1958; Okada, 1985; Davis, 1986).
This might have had a strong effect on the medium around the pressure source.
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