Figure 2: Data from a local meteorological station, glider and HF radar. | Nature Communications

Figure 2: Data from a local meteorological station, glider and HF radar.

From: Stratified coastal ocean interactions with tropical cyclones

Figure 2

(a) Tuckerton WeatherFlow, Inc. station 10 m wind speed (orange) and direction from (black) with vertical black dashed line/label indicating the time/value of the minimum air pressure corresponding to landfall time on 28 August at 935 GMT. (b) Temporal evolution and vertical structure of the glider temperature during storm conditions with lines indicating top (black) and bottom (magenta) of thermocline. (c) Cross-shelf currents (positive onshore, negative offshore) for the surface layer (red) from CODAR HF Radar, depth-averaged (green) from the glider and bottom layer (blue) calculated from the depth-weighted average of the HF radar and glider velocities. (d) Same as c but for along-shelf currents (positive up-shelf northeastward and negative down-shelf southwestward).

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