Swash, groundwater and sediment transport processes on a gravel beach
The morphodynamics of a steeply sloping gravel beach in the south western UK (tanβ = 0.15–0.2; d50 = 6 mm; ξb = 1–4) were measured during low energy wind-wave conditions (Hb < 0.5 m). Measurements of water depth, groundwater-level, waves and currents, concurrent with observations of morphological...
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| Format: | Default Thesis |
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2005
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| Online Access: | https://hdl.handle.net/2134/34493 |
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