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The use of HF radar surface currents for computing Lagrangian trajectories: benefits and issues

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Academic year: 2019

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Figure

Figure 1. Map of the area of study showing the location of the two radar stations (Tannum Sands and Lady Elliot Island) and of the three ADCP surface current vectors (26/10/07 at 9:40 am; local time) produced by the mooring stations (small squares; see det
Figure 2. Schematic diagram of the two radial velocity components (v1, �1) and (v2, �2) and the resultant surface current velocity vector magnitude and direction (v, �)
TABLE I PREDICTED
Figure 5 (aand mooring tracking coordinates for the tracks starting at H1, H2 and H3 stations

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