Criccieth local scale coastal envroinment Case Study Flashcards
Aim
to investigate impacts of coastal processes on coastal landforms and people along the Criccieth coastline
hypothesis
the size of the beach will increase with distance across Criccieth bay, this is because of longshore drift
secondary research
what longshore drift is
how it enlarges bay in the west
what controls the wave strength and LSD direction (fetch, orientation in relation to SW prevailing wind)
sampling techniques used (choosing profile locations)
stratified sampling: split beach into 3 sections, aimed to carry out 2 beach profiles in each area
justification: better overall view of beach, using systematic could only have measured sites at one small area of beach. also helped us avoid dangerous sections of the beach
sampling techniques used (collecting data from each profile)
systematic sampling: measured width of beach and took readings at 5 metre intervals
justifiction: easy to carry out, accurate and unbiased. using stratified we could have left out areas, leading to biased and inaccurate results
qualitative evidence
the beach at site 3 was much smaller because: the SW prevailing wind met the orientation of the coastline at a 50% angle, meaning LSD was particularly strong at removing material
the groynes caused beach starvation via LSD causing less sediment to reach parts of the bay further along the beach
beach scour: when waves hit the sea wall, they can rebound and take sediment of the beach
qualitative evidence (site one)
the beach at site one was not the smallest as the break water created low energy conditions and encouraged greater levels of deposition
qualitative evidence (site 12)
the beach at site 12 was alot larger because LSD travels in an eastern direction due to the SW prevailing wind in relation to the coastline, aswell as the erroding cliffs in the middle providing more sediment.
Graig Duu headland also limits the amount sediment that can be removed by LSD
graphical representation of quantitative data (what was the TEAR)
trend:beach becomes larger as you get closer to east of the bay
example: over doubles in size between sites 3 and 12.
anomaly: site 1 should have been the smallest but site 3 was
range: 5.30 - 2.15 = 3.15
justification: by drawing each beach profile on the same graph you can make easy and direct comparisons between each beach section
method one (collection of quantative primary data)
stratified sampling was used to select each beach measurement site. A 50 m measuring tape was used to measure from the top of the beach to the sea. then a dumpy level was set up and made level by manipulating the legs of the tripod until the spirit level indicated it was level. one member of the team held the 5m staff up at the top of the beach. a reading was taken by looking to see were the crosshairs lined up with the staff. this figure was written down. another reading was taken in the same way 5m further down the beach. the second figure was subtracted from the first to show how the height of the beach had changed. this was repeated every 5m until we reached the sea.
justification of method one
helps to provide quantative data so each section of beach can be easily compared. we can therefore sea how the height of each section of the beach changes and see whether our hypothesis was correct. this method was also easy to carry out and provided accurate data.
method two (collection of qualitative primary evidence)
took photos and wrote down how this explained the data we were collecting e.g groynes/breakwaters
justification: helped us collect data that we couldnt have got from the beach profile data alone. this method helps us interpret why some sections of beach were bigger than others.
spearmans rank
formula: 1 - ((6*d^2)/(n^3-n))
ranked distance across the bay from largest to smallest and did the same with beach width. we took one from the other to find the difference and then squared the resulting value to get d^2 = 16.
N=12 as we took readings from 12 sites. plugging these numbers in gives us 0.9441
justification: clearly shows correlation with no interpretation
limitations: shows correlation but not causation
level of signifance on degrees of freedom chart is 0.1% so there is a 99% chance of correlation
evidence for/against hypothesis (quantitative)
for: beach profile diagram shows beach become larger in the east. also spearmans rank shows positive correlation between distance across the bay and beach size.
against: site one was the furthest west but not the smallest
evidence for/against hypothesis (qualititative)
for: photograph showing beach larger in east due to Graig Duu, which acts as a massive groyne
against: photograph showing site one wasnt the smallest, suggesting an anomaly