Impacts of Interannual Ocean Circulation Variability on Japanese Eel Larval Migration in the Western North Pacific Ocean
Fig 3
(a) Time series of PTO (black) and NEC bifurcation latitude (NECBL, magenta; Qiu and Chen, [44]) anomaly. Red and blue arrows mark the chosen years for positive and negative PTO, respectively. Lower panels show 20-year (1993–2012) composite surface current anomaly trajectories (ms-1) and sea surface height anomalies (m) for (b) the positive and (c) the negative PTO years calculated from the JCOPE2 reanalysis.