Wednesday, 23 July 2008

Profile response C5 and C6



The profile response (before/after) of series C5 and C6 (longer period waves, low and high lagoon respectively). As with the runs with shorter wave periods, a low lagoon level promoted beachface accretion. The profile change associated with a higher lagoon level (C6) was less substantial, with some crestal accretion and relative depletion in the region of wave breaking (exit point effect?). C6 destroyed the subtidal ripple field

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