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Where is longshore drift coming from?

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Synchronised kite flying.

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11. Sediment size at Eastern side of jetty

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11. Sediment size at Eastern side of jetty

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Closest to water's edge. The line of debris of darker stones, peddles and leaves represent where the swash came up to.

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8. Fieldwork site - Jetty at Dalgeria Green

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8. Fieldwork site - Jetty at Dalgeria Green

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Eastern side of jetty

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10. Sediment size along Eastern side of jetty

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10. Sediment size along Eastern side of jetty

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1 step towards the water.

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7. Fieldwork site - Jetty at Dalgeria Green

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7. Fieldwork site - Jetty at Dalgeria Green

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Western side of jetty

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9. Sediment size along Eastern side of Jetty

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9. Sediment size along Eastern side of Jetty

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Furthest from water's edge.

Shoe used as scale.

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Where's the longshore drift come from?

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Singapore doesn't really use groynes as a coastal protection measure, but there are cases where pipes and jetties protuding out to the sea have also helped serve as groynes, reducing the rate of longshore drift along the coast.

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The seawall gives way to a stepped seawall. In some areas, stepped seawalls are used instead of normal seawalls to resolve the problems of the powerful backwash.

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Seawall to protect the backshore! Note the difference between backshore and riprap.

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Brownish waters as waves break on the shore. Sign of erosion - brownish water is sand and finer sediments suspended in the water.

Grasses at backshore also help stabilise the sand - sometimes used as coastal protection measure

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2 Coastal protection measures (breakwater and riprap)

Teeny Weeny cliffs (in background) show evidence of erosion

Barriers to stop people from going to the edge