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Fig. 11 | Progress in Earth and Planetary Science

Fig. 11

From: Drastic thickening of the barrier layer off the western coast of Sumatra due to the Madden-Julian oscillation passage during the Pre-Years of the Maritime Continent campaign

Fig. 11

Time-depth sections of a SLA (cm), b SST, c the vertical motion averaged between 45 and 155 m (× 103 cm/s), d the depth of the 20 °C isotherm (m), e the salinity anomaly from the temporal mean for October–December averaged between 45 and 155 m, and (f) BLT (m) with ECCO2. The surface westerly wind speed (blue contours for every 1 m/s) is shown in a and b. The ILD (white contours for every 10 m) is shown in f. The bold black line in each panel indicates the fixed observation period of R/V Mirai

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