3.1.3.1 Coasts as Natural Systems Flashcards
What type of system is the Coastal system
Open
Sediment Cells
Divided sections of coastline that are self contained for the movement of sediment.
This means that the processes going on in one cell doesn’t affect the system of another.
They are usually divided by headlands.
Coastal Inputs
- Marine (waves, tides)
- Atmosphere (sun, wind speed / direction)
- Humans (pollution, defences)
Coastal Outputs
- Sediment transfer (erosion and LSD out of system)
- Evaporation
Coastal Stores
- Beaches
- Spits
- Bars and Tombolos
- Headlands and Bays
- Cliffs, etc
Coastal Flows / Transfers
- Mass-movement processes
- Longshore drift
- Weathering
- Erosion
- Transportation
- Deposition
Dynamic Equilibrium
Coastal systems are generally in dynamic equilibrium which is where there is a balance between the inputs and outputs. A change in one often causes negative feedback that restores the equilibrium of the system. However positive feedback does also occur and this creates a new equilibrium.
Positive feedback loop in coasts
A storm causes more erosion then usual
The ridge of a sand dune is breached
The ridge is then undercut by wind erosion
This breaks up the dune making it more likely to be eroded
Negative feedback coasts
Sediment is eroded from the beach during a storm
Sediment is deposited offshore forming an offshore bar
Waves now break before reaching the beach, dissipating their energy and reducing further erosion when they reach the beach
When the storm calms normal wave conditions rework sediments from the offshore bar back to the beach
The beach is in dynamic equilibrium