CASE STUDY - Christchurch bay Flashcards
(6 cards)
management strategies implemented (intentional)
- timber groynes at Hengistbury Head and Milford-on Sea –> interrupts LSD
- sea walls and Friars Cliff and Milford-on-Sea –> reduce erosion and protect high-value infrastructure
- cliff drainage and vegetation –> reduce mass movement and cliff erosion
- beach nourishment at Hurst Spit —> maintain its role as floor barrier
reasons for the management strategies implemented
- Economic: £50m+ real estate, e.g., holiday homes at Naish and golf course.
- Environmental: Protect SSSI (Naish), prevent erosion of natural defences.
- Social: Tourism value (e.g., Christchurch) and coastal access.
Impacts of management strategies on PROCESSES & FLOWS BUDGET
- groynes interrupt LSD - starving Hurst Spit of sediment
- cliff stabilisation (drainage and rip rap at Barton-on-Sea and Highcliffe) - reduces natural cliff erosion - leading to lower sediment input into sediment budget
- sediment stored at groyned beaches (eg Milford-on-Sea) but downdrift areas are depleted of sediment
- beach nourishment at Hurst Spit artificially maintains sediment levels but requires regular replenishment - ££ and not sustainable in the long term
Impacts of management strategies on ENERGY BUDGET
- sea walls at Friars Cliff and Milford-on-Sea reflect wave energy
- rip rap (Naish Beach) allows percolation of swash energy - reducing reflected wave power and slows erosion
- groynes interrupt wave-driven longshore transport, trapping sediment but reducing downstream movement and energy redistribution
Impacts of management strategies on CHANGING LANDFORMS
HURST SPIT
- would normally grow but starved of sediment due to groynes
- maintained by artificial nourishment
- not retreating - holding the line
HIGHCLIFFE CLIFFS
- stabilised with rip rap + veg
- reduced slumping but blocks sediment supply from cliff
- less upper beach formation - natural dynamic processes disrupted
NAISH BEACH
- more natural with embryo dunes and less hard engineering
- cliff is steeper due to rapid erosion of clay
FRIARS CLIFF
- sea wall reflected wave energy, steepening the beach profile and increasing basal erosion
Consequences of these changing landscapes
- terminal groyne syndrome - east of Barton-on-Sea –> bc upstream groynes rap sediment so more erosion downstream –> stepped coastline (defended sections contrast with defended ones)
- more embayment in unmanaged areas –> where clay cliffs erode rapidly no protection = high erosion = recessed coastline
- fragmented coastline –> some are heavily managed like Friays Cliff and Milford, others are ‘do nothing’ zones. –> loss of sediment cell balance