Fig. 1 | Nature Communications

Fig. 1

From: The role of enhanced velocity shears in rapid ocean cooling during Super Typhoon Nepartak 2016

Fig. 1

Satellite and buoy NTU1 observations of Nepartak. a Satellite SST difference between pre-storm SST (5 July) and post-storm SST (8 July) with the typhoon track indicated by the gray line. Dashed circles and white contours in a indicate the radius of the Beaufort scale 10 wind and sea level anomalies of −0.1 and −0.2 m. Buoy NTU1 observed parameters: b air pressure (black line) and wind speed (blue line); c temperature in the upper 300 m; d meridional current velocity Vcurr at 75 m (black line) and meridional wind velocity Vwind (red line). The two red vertical lines in bd mark the beginning (left) and end (right) of the forced period. The black curve in c is the 27.2 °C isotherm. e Observed (red line), simulated (blue line), and pre-storm (black dashed line) temperature profiles at times 1–6 as indicated by the vertical black dashed lines in c and d. Black lines in e mark the mixed layer depth. The black vertical line in bd marks the time of minimum sea level pressure

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