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Lagrangian transport in a microtidal coastal area: the Bay of Palma, island of Mallorca, Spain

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Figure

Fig. 1. Bathymetry contours (in meters) of the model domain. Theblack box indicates the Bay of Palma and the inset graphics give thegeographical location of Mallorca Island in the western Mediter-ranean Sea.
Fig. 2. (a) Complete time series throughout October of the zonal(top panel) and meridional (bottom panel) of the spatial average ofthe surface velocity field (black line)
Fig. 4. Spatial distribution of the time average of 6-hourly FSLEs maps over different months and at different layers: (a) October at surfacelayer, (b) July at surface layer, (c) July at bottom layer.
Fig. 6. Average of 15 subsequent (started at t0 values separated 18 h)estimations of N(t), the number of particles remaining in the Bay ofPalma at least for a lapse of time t after release at t0
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