Coasts PowerPoint Flashcards
What are the physical factors influencing coastal landscapes?
- winds: speed, direction and frequency
- waves: wave formation, development and breaking
- tides: tidal cycles and range
- currents: global patterns
- geology: lithology and structure
the energy of a wave is dependent on
the strength of the wind, its duration and the length of fetch
the source of energy for coastal erosion and sediment transport is
wave action
wave energy is generated by
frictional drag of winds moving across oceans; and is a result of fetch
fetch is
the length of open water which the wind can blow unobstructed
how do ocean waves build
Ocean waves build in response to the shear of wind blowing over the water surface. Higher-energy wind yields higher-energy waves. Within a passing wave, water follows a circular path. The circle radius decreases with depth.
how do waves break
As a wave approaches shore, friction slows its base.
Water motion in the wave becomes more elliptical, the wave oversteepens, and it crashes ashore as a breaker.
what is tidal range
Vertical distance between the high tide and the low tide
tidal range- place with highest tidal range
The Bay of Fundy, on the east coast of Canada, is often stated to have the world’s highest tides because of its shape, bathymetry, and its distance from the continental shelf edge
A max range of 16.8 m has been recorded
what are spring tides
Spring tides occur twice each lunar month all year long without regard to the season
what is a neap tide
When the sun and moons are at right angles to each other, there is least gravitational pull, meaning the tidal range is at its lowest. The neap tide occurs 7 days after the spring tide.
Two factors that will affect the horizontal distance over which the shoreline can migrate between high and low tide
- Position of moon (neap and spring tides related to tidal range)
- Slope of shoreline- if tidal range large and slope gentle the position of the shoreline can move a long way leaving a broad tidal flat exposed to the air
When a tidal current moves towards the land and away from the sea, it…
floods
when it moves toward the sea away from the land it…
ebbs
Tidal currents that ebb and flood in opposite directions…
results in horizontal motion producing currents called ‘rectilinear’ or ‘reversing’ currents.