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Summary A-level Geography Coasts Revision Notes $13.78   Add to cart

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Summary A-level Geography Coasts Revision Notes

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In-depth notes for the whole topic of coasts following the AQA Coasts syllabus breakdown. All subtopics have examples located in the UK. The local scale case study is the Holderness Coast in the UK. The Case Study beyond the UK is Odisha, India. There are other case studies possible in the syllabus...

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  • November 2, 2024
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‭AQA A-level Coasts Knowledge Booklet‬




‭Coastal Systems‬
‭1.‬ ‭Coastal Systems‬
‭●‬ ‭Simple system approach of a coast (inputs, outputs, stores, transfers and processes)‬
‭●‬ ‭Sediment Budget refers to the gains and losses of sediment within a sediment cell‬
‭○‬ ‭Positive sediment budget:‬‭more inputs than outputs‬‭of sediment leading to a‬
‭sediment‬‭surplus‬‭which creates a‬‭wider beach‬
‭■‬ ‭Human management strategies eg. groynes can help accumulation‬
‭of sediment (surplus)‬
‭○‬ ‭Negative sediment budget:‬‭more outputs than inputs‬‭cause a sediment‬
‭deficit‬‭which creates a‬‭narrower beach‬
‭■‬ ‭Sediment is lost via LSD, wind and sea removal or human‬
‭interference‬
‭○‬ ‭Neutral sediment budget: inputs = outputs so the beach is in equilibrium‬

‭●‬ ‭Sediment cells AKA littoral cells are the area within sediment moves (11 in UK)‬
‭○‬ ‭They are normally‬‭closed systems‬‭since they contain‬‭the sediment within an‬
‭area‬
‭■‬ ‭This area is often kept isolated between headlands‬
‭○‬ ‭These cells can become open systems during extreme natural variation eg.‬
‭storms which can carry sediment around a headland‬
‭■‬ ‭When sediment is permanently removed from an area the area‬
‭becomes a‬‭sediment sink‬

‭●‬ ‭Feedbacks in the Coastal System‬
‭○‬ ‭Positive feedbacks - when the change is amplified‬
‭■‬ ‭Sea levels rise → vegetation on sand dunes is removed → more‬
‭erosion of sand dunes → wind is able to erode more → sand dunes‬
‭become fully eroded‬
‭○‬ ‭Negative feedbacks - when the change is restored‬
‭■‬ ‭Erosion of sand dune → sand transported by the waves to form‬
‭off-shore bar → incoming waves are slowed by obstacles →‬
‭deposition occurs → sand dunes build back up‬

‭●‬ ‭Types of equilibrium in a coastal system‬
‭○‬ ‭Steady-state - energy entering = energy leaving so the coast stays the same‬
‭all year round‬
‭○‬ ‭Dynamic equilibrium - change is gradual, the system is constantly adapting to‬
‭find an equilibrium‬

, ‭○‬ M
‭ etastable equilibrium (only for coasts) - dramatic events change the‬
‭equilibrium of the coast eg. a storm‬




‭2.‬ ‭Energy in the Coastal System‬
‭●‬ ‭Wind energy‬
‭○‬ ‭Solar energy creates areas of high and low pressure. When air moves from‬
‭high to low pressure wind is formed. Wind blows over the water to form‬
‭waves. (Air always moves to the area of lowest pressure)‬
‭●‬ ‭Wave energy‬
‭○‬ ‭Waves are bodies of water that move in circular motions between the crest‬
‭and trough. Energy is transferred between the crest and trough to create‬
‭oscillatory waves‬
‭○‬ ‭In shallow water, friction slows the circular motion but the upper motion‬
‭continues to create a transition (breaker wave)‬
‭○‬ ‭Many factors affect the energy of a wave:‬
‭■‬ ‭atmospheric pressure → areas of low pressure eg. north atlantic =‬
‭higher energy waves‬
‭■‬ ‭wind direction → prevailing winds = higher energy waves‬
‭■‬ ‭fetch → the longer the fetch = higher energy waves‬
‭■‬ ‭storm surges → intense areas of low pressure = higher energy waves‬

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