Figure 1: Scientific Reports

Figure 1

From: On the shape and likelihood of oceanic rogue waves

Figure 1
Figure 1

Frequency (f) - direction (θ) wave spectrum S during the stereo acquisitions, and for the Draupner case (throughout the paper we use flow direction of the wave energy). Station P spectra (SP1 and SP2) were derived from the directional WaveRider buoy parameters; Acqua Alta (AA1 and AA2) and Black Sea (BS1) spectra were derived from stereo data using the extended maximum entropy principle method. The Draupner spectrum was computed by the wave model ECWAM at 14-km resolution forced with ECMWF winds at 9-km resolution22. Given the wide range of energy levels, axis limits and color-scale change among panels.