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Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

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. 10

Averaged horizontal distribution of a SSH (cm), b SST (°C), 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 averaged between 45 and 155 m, and f the BLT (m). The surface wind vectors with JRA55 are shown in a and b. The ocean current vectors averaged between 45 and 155 m with ECCO2 are shown in ce. The sections in Fig. 11 are plotted along the black solid line

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