File:InnerClosureDepth.jpg

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Summary

Schematic illustration of the closure-depth concepts of Hallermeier and Kraus et al. The active coastal zone is represented here by the upper shoreface, where cross-shore sediment exchange occurs frequently over timescales of years to decades. The inner closure depth is located where the mean beach profile converges with the storm profile associated with wave conditions exceeded for approximately 12 hours per year.

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current20:28, 6 August 2026Thumbnail for version as of 20:28, 6 August 2026884 × 405 (48 KB)Dronkers J (talk | contribs)Schematic illustration of the closure-depth concepts of Hallermeier and Kraus et al. The active coastal zone is represented here by the upper shoreface, where cross-shore sediment exchange occurs frequently over timescales of years to decades. The inne...
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