Figure 4
From: Variability of the nutrient stream near Kuroshio's origin
The poleward transports of (a) water, (b) N and (c) P and averaged (d) N and (e) P concentrations along the Kuroshio path. The data of KTV1 were calculated between 0–250 m and 0–1000 m4. These transports of PN, TK, ASUKA, and 137E were estimated2,3 for the layers between the surface and σθ = 25.5(280–350 m) or 27.3(850–1100 m).
