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Coastal Processes |
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Sediment transport in the nearshore zone (close to the beach), especially during storm conditions, is
predominantly from the beach to offshore with along-shore wave energy being only 10% of the onshore-offshore
component. A net southward along-shore drift is dominant, although
localised drift reversals can occur under different wave climates. Wave driven along-shore drift
occurs predominantly in the surf zone, whilst tidal currents may transport a significant amount
of material offshore of the surf zone.
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What happens during a storm? |
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During a storm large waves wash beach material offshore. Because storms occur on a regular basis during the winter, beach levels fluctuate on a seasonal basis. |
gorleston beach before storm (Feb 2000)
gorleston beach after storm (Apr 2000) |
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Summer wave conditions move sand onto the beach Winter storm waves move sand offshore |
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| At Gorleston this process is not in balance, and as a result more material is carried offshore than onto the beach. |
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Has Gorleston beach always had a problemFollowing the construction of the harbour piers at Great Yarmouth, and their extension in the
early 1960's less beach material was able to reach Gorleston beach from the north. Because
the net sediment transport is in a southerly direction the harbour piers trap beach material. |
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