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Progress in Earth and Planetary Science
Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

From: Deep-sea bottom-water environment change caused by sediment resuspension on the continental slope off Sanriku, Japan, before and after the 2011 Tohoku Earthquake

Fig. 4

Vertical profiles of pressure (a), potential temperature (b), salinity (c), LTA (d), DO (e), AOU (f), NO3 (g), PO4 (h), and DIC (i) as functions of potential density (σθ) and the location map (j) by using the cruises (Table 1). Colored circles denote the latitude of sampling locations. Lines show the studied isopycnal surfaces (27.38σθ: red; 27.56σθ: blue)

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