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Table 1 Correction coefficient \(\beta\) used to balance the seismic moment calculated from geodetic strain rates to that of past large earthquakes

From: Time-independent forecast model for large crustal earthquakes in southwest Japan using GNSS data

  \(\dot{\gamma }\)
(Eq. 1)
\(\mathrm{Max}(\left|{\dot{\varepsilon }}_{h1}\right|, \left|{\dot{\varepsilon }}_{h2}\right|)\)
(Eq. 2)
\(\mathrm{Max}(\left|{\dot{\varepsilon }}_{h1}\right|, \left|{\dot{\varepsilon }}_{h2}\right|, \left|{\dot{\varepsilon }}_{h1}+{\dot{\varepsilon }}_{h2}\right|)\)
(Eq. 3)
UNI model 0.193 0.125 0.121
VARI model 0.198 0.130 0.126