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Three sub-Plinian eruptions took place on 26–27 January 2011 at Shinmoe-dake volcano in the Kirishima volcanicgroup, Japan. During this event, GPS and tiltmeters detected syn-eruptive ground subsidence approximately7 km to the WNW of the volcano. Starting in March 2011, we conducted broad-band magnetotelluric (MT) measurementsat a site located 5 km NNW of the volcano, beneath which the Shinmoe-dake magma plumbing systemmay exist. In addition, temperature monitoring of fumaroles and hot-springs near the MT site was initiated inJuly 2011. Our MT data record changes in apparent resistivity of approximately ±5%, along with a ±1◦ phasechange in the off-diagonal component of the impedance tensor (Zxy and Zyx ). Using 1-D inversion, we inferthat these slight changes in resistivity took place at relatively shallow depths of only a few hundred meters, at thetransition between a near-surface resistive layer and an underlying conductive layer. Resistivity changes observedsince March 2012 are correlated with the observed temperature increases around the MT monitoring site. Theseobservations suggest the existence beneath the MT site of pathways which enable volatile escape

Magnetotelluric and temperature monitoring after the 2011 sub-Plinian eruptions of Shinmoe-dake volcano