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First, we assumed a spherical pressure source (Fig. 2a).
Upward changes represent extension by inflation of the pressure source.
In positive pressure mode, the compressor is pressure source.
a Modeled pressure source based on GEONET data alone.
The star is the location of the pressure source.
We interpret this change as having been caused by a shallow pressure source.
Fig. 8 Result of the inversion estimating the point pressure source beneath the Owakudani.
This might have had a strong effect on the medium around the pressure source.
We examined two source types, a spherical pressure source and a tensile crack source.
The circle shows the pressure source estimated with campaign GNSS data (Sphere2 in Fig. 6).
We used the following procedure to estimate four unknown parameters for each pressure source.
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