Wave And Sea Levels Flashcards
What are high energy coastlines?
High-energy coastlines are associated with more powerful waves, so occur in areas where there is a large fetch. They typically have rocky headlands and landforms and fairly frequent destructive waves. As a result these coastlines are often eroding as the rate of erosion exceeds the rate of deposition.
What are low energy coastlines?
Low-energy coastlines have less powerful waves and occur in sheltered areas where constructive waves prevail and as a result these are often fairly sandy areas. There are landforms of deposition as the rates of deposition exceed the rates of erosion
What does the size of the wave depend on?
The size of a wave depends on various factors including:
- The strength of the wind
- How long the wind has been blowing for
- Water depth
- Distance of fetch
What are the features of constructive waves?
▪ Strong swash, weak backwash
▪ Low wave height, long wavelength
▪ Low frequency
▪ Depositional
Features of destructive waves?
▪ Strong backwash, weak swash
▪ High wave height, short wavelength
▪ High frequency
▪ Erosional
What can cause short term sea level change?
- High tide and low tide - a daily phenomena due to the gravitational pull of the Moon.
- Wind strength and direction - these can change causing a change in sea level for a couple of minutes or longer
- Atmospheric pressure - the lower the pressure, the higher the sea levels.
What can cause long term sea level rise?
Isostatic - localised sea level change
Isostatic sea level change could be due to post-glacial adjustment (glaciers weigh down the land beneath, and so the land subsides until it melts).
Tectonic activity (such as earthquakes and volcanic eruptions) may cause land subsidence, therefore causing isostatic sea level increase.
Eustatic rise - Global sea level change
Eustatic rise is due to thermal expansion. Water expands when it gets warmer, and so the volume of water increases which as a result, sea levels increase. This is due to Global Warming.