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Particle tracking has been performed in order to study cross shelf mixing and transport.
Concurrently, we sampled zooplankton at 16 stations along a cross shelf transect in the vicinity of Triangle Island.
The genetic structure of A. polyacanthus was consistent with these cross shelf current patterns.
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Species cross-shelf distributions were often bimodal.
One aim of the program was to determine the strength and effectiveness of local cross-shelf transport processes.
In both cases, cross-shelf currents control sediment distribution and accumulation, not location or amount of primary eolian input.
Brodie et al. (2007) reported on a long-term Great Barrier Reef chl-a monitoring program which demonstrated a significant cross-shelf difference in chl-a concentrations.
Discrete regional cross-shelf transects were monitored within each region during the wet season (ca. December to April) from 2006 to 2013.
Effective cross-shelf transport occurs only when (1) internal tides at the shelf break are strong and (2) subtidal currents flow strongly downcoast.
For both of these scenarios, a large cross-shelf sanctuary zone at the widest part of SIMP was an important requirement for achieving representation.
The extent of the primary water type (fp) was variable across regions and cross-shelf, reflecting the intensity, duration, and constituent concentrations of the river discharge, but limited to a small near-shore zone (< 10 km across the shelf).
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