Fig. 2From: Deep-sea bottom-water environment change caused by sediment resuspension on the continental slope off Sanriku, Japan, before and after the 2011 Tohoku EarthquakeVertical distributions of light transmissometer anomaly (LTA) values measured during cruises MR12-E02 (a, e, and i), BO13-20 (b, f, and j), KS-15–15 (c, g, and k), and KS-17-J05 (d and h) off Ohtsuchi Bay, Onagawa Bay, and Sendai Bay (l). Contours of LTA are every 1%Back to article page