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Salty lil beach shirt
Conversely, the beach profile is lower in the storm season due to the increased wave energy, and the shorter periods between breaking wave crests. Higher energy waves breaking in quick succession tend to mobilise sediment from the shallows, keeping it in suspension where it is prone to be carried along the beach by longshore currents, or carried out to sea to form longshore bars, especially if the longshore current meets an outflow from a river or flooding stream. Salty lil beach shirt The removal of sediment from the beach berm and dune thus decreases the beach profile. In tropical areas, the storm season tends to be during the summer months, with calmer weather commonly associated with the winter season. If storms coincide with unusually high tides, or with a freak wave event such as a tidal surge or tsunami which causes significant coastal flooding, substantial quantities of material may be eroded from the coastal plain or dunes behind the berm by receding water. This flow may alter the shape of the coastline, enlarge the mouths of rivers and create new deltas at the mouths of streams that had not been powerful enough to overcome longshore movement of sediment.
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The sand deposit may extend well inland from the berm crest, where there may be evidence of one or more older crests resulting from very large storm waves and beyond the influence of the normal waves. At some point the influence of the waves on the material comprising the beach stops, and if the particles are small enough , winds shape the feature. Where wind is the force distributing the grains inland, the deposit behind the beach becomes a dune. These geomorphic features compose what is called the beach profile. The beach profile changes seasonally due to the change in wave energy experienced during summer and winter months. In temperate areas where summer is characterised by calmer seas and longer periods between breaking wave crests, the beach profile is higher in summer. The gentle wave action during this season tends to transport sediment up the beach towards the berm where it is deposited and remains while the water recedes. Onshore winds carry it further inland forming and enhancing dunes.
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