Fig. 6From: Deep-sea bottom-water environment change caused by sediment resuspension on the continental slope off Sanriku, Japan, before and after the 2011 Tohoku EarthquakeTime series of DO in the bottom water at the deep-sea station (~ 1000 m depth) off Otsuchi Bay (Fig. 1a) before and after the events of the large earthquakes (purple double lines): February 17, 2015 (Ev1, Fig. 1a), September 17, 2017 (Ev2, Fig. 1a), and July 7, 2018, off then Boso Peninsula (Ev3). Dashed and bold lines refer to the 9-day mean values before and after the large earthquakes, respectivelyBack to article page