Coastal Energy Flashcards
The driver
. The initial energy input for the coastal system is from the sun
. The sun’s energy causes different air pressures (due to different rates of heating) which creates wind
. This wind then generates waves, the main form of energy at the coast.
Wind energy
. Wind is formed by air moving between areas of different pressure (from high to low) along a pressure gradient
. The steeper the gradient the faster the wind moves
. So areas with large pressure gradients experience strongest winds
Fetch
. Area of ocean or lake surface area which the wind blows in an essentially constant direction
. Fetch determines wave size
. The longer the fetch the longer the wave
Wind strength
. The stronger the winds, the larger the force and therefore a bigger wave and greater friction on sea surface
. Wind gives waves energy
Direction of the wind
. The greater the wind velocity the longer the fetch and the greater duration the wind blows, then more energy is converted to waves and the bigger the waves
. Longer the wind blows the larger the wave
. If wind speed is slow the resulting waves will be small regardless of fetch or duration
. Strength = biggest energy supply
Constructive waves
. Strong swash . Weak backwash . Low wave in proportion to length . Adds material to coastline . Formed by distant weather systems
Destructive waves
. Common during winter storms . Strong backwash . Weak swash . High wave in proportion to length , tall breaks which breaks downwards with great force . Removes material from the coastline . Generally steep beach profile
Formation of waves
. Waves are created by energy passing through water, causing it to move in a circular motion
. However, water does not actually travel in waves
. Waves transmit energy, not water, across the ocean and if not obstructed by anything, they have the potential to travel across an entire ocean basin
. Waves are most commonly caused by wind
. Wind-driven waves, are created by the frictional drag between wind and surface water
. As wind blows across the surface of the ocean, the continual disturbance creates a wave crest
. As the wave approaches the shore disturbance to the circular motion beneath the surface leads to more
horizontal wave movement and the wave breaks.