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of Temporal variation in the resistivity structure of the first Nakadake crater, Aso volcano, Japan, during the magmatic eruptions from November 2014 to May 2015, as inferred by the ACTIVE electromagnetic monitoring system

Additional file 1. Details of inversions and sensitivity analyses.

Additional file 1: Figure S1. Depth-averaged conductivity anomaly (relative to annual mean) for each of the four seasons. The full range in the data are, respectively, −0.660–−0.556 (S/m), −0.471–−0.317 (S/m), −0.511–−0.721 (S/m), −0.502–−0.594 (S/m).

Additional file 2. Supplement document comparing results here with results from a previous study.