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Flushing time of solutes and pollutants in the central Great Barrier Reef lagoon, Australia

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Figure

Fig. 1.Location of six conductivity–temperature–depth (CTD) transectsVI is the transect of Wolanski and Jones (1981) taken in 1979
Fig. 2.Mechanisms that can cause dispersion of solutes from the Great Barrier Reef lagoon: (shear; (a) windb) meanders of the East Australia Current onto the continental shelf; (c) river plumes; (d) hypersalineplumes; and (e) wind driven onshore surface flow and offshore bottom flow.
Table 1.Measurements of long-term averages of longshore currents at various locations in the Great Barrier Reef lagoonMean current is positive if directed northward, x and L is defined in Fig
Table 3.The summary of conductivity–temperature–depth (CTD) transects I to V measured in 2005
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