Fig. 2
From: The role of enhanced velocity shears in rapid ocean cooling during Super Typhoon Nepartak 2016

Buoy NTU2 observations of Nepartak. a Air pressure (black line) and wind speed (blue line); b temperature in the upper 300 m; c meridional current velocity Vcurr at 25 m (thick black line) and 75 m (thin black line), and meridional wind velocity Vwind (red line). The two red vertical lines in a–c mark the beginning (left) and end (right) of the forced period. The black curve in b is the 27.2 °C isotherm. d 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 b and c. Black lines in d mark the mixed layer depth. The black vertical line in a–c marks the time of minimum sea level pressure. e Velocity shear square \(\bar S^2\) (red line), four times of buoyancy frequency square 4\(\bar{N}^{2}\) (blue line), and \(\bar {S}^{2}{/}4\bar N^{2}\) (black line). The two white lines in b indicate the depths of the two current meters measured by the pressure sensors of the current meter