Fig. 2: Reservoir thermodynamics and surface observations.
From: Steam caps in geothermal reservoirs can be monitored using seismic noise interferometry
a Decadal pressure and temperature variations from the iTOUGH2 hydrogeological model of the area36 at the three locations numbered in Fig. 1b. b Same for the steam ratio. c Modeled seismic velocity variations for P- and S-waves obtained from the rock physics model (see Methods subsection “Rock physics model”). d Cumulative near-up surface displacement during the COSEISMIQ project (black line) and the observed \(\triangle v/v\) (dark red line) together with their annual rate.
