Inputs Flashcards

1
Q

fetch

A

the distance of open water over which the wind blows uninterrupted by major land obstacles

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2
Q

the length of fetch determines…

A

the magnitude and energy of the waves reaching the coast

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3
Q

waves are created by…

A

the transfer of energy from the wind blowing over the sea surface (frictional drag)

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4
Q

wave frequency/period

A

the time for 1 wave to travel the distance of one wavelength or the time between 1 crest and the following crest passing a fixed point

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5
Q

swash

A

the rush of water running up the beach

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6
Q

backwash

A

any water running back down the beach towards the sea

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7
Q

waves are driven by

A

the wind

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8
Q

negative feedback

A

constant cycle of: constructive waves build up beach (steeper profile) which encourages waves back as destructive, with time destructive moves material towards sea, reducing angle, encouraging more constructive waves

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9
Q

wave refraction

A

when waves approach a coastline that is not regular shape, they are refracted and become increasingly parallel to coastline

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10
Q

current

A

the permanent or seasonal movement of surface waves in seas and oceans

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11
Q

longshore currents (littoral drift)

A

most waves approach at an angle to coastline so generates flow of water running parallel to shoreline

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12
Q

rip currents

A

strong currents moving away from shoreline developed when seawater is piled up by incoming waves

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13
Q

upswelling

A

movement of cold water from deep in the ocean towards surface as more dense cold water replaces the warmer surface water and creates nutrient rich colder ocean currents

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14
Q

tides

A

the periodic rise and fall in the level of the sea

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15
Q

cause of tides

A

gravitational pull of sun and moon (moon has greater force as closer) so moon pulls water towards it creating high tide and compensatory bulge on opposite side of Earth

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16
Q

as the moon orbits the earth…

A

high tides follow it

17
Q

tidal range

A

the difference in height of seawater at high and low tide but not fixed due to tidal cycles

18
Q

tidal range determines…

A

upper and lower limits of erosion and deposition

the time each day the littoral zone is exposed and open to subaerial weathering

19
Q

low tidal ranges

A

along coast of Mediterranean Sea which restricts wave action to narrow width

20
Q

high tidal ranges

A

parts of British Isles which gives wide zone of wave attack so forming wide wave-cut platforms

21
Q

macrotidal

A

more than 4m

22
Q

mesotidal

A

2-4m

23
Q

microtidal

A

less than 2m

24
Q

sources of sediment

A
streams/rivers into sea
estuaries
cliff erosion
offshore sand banks
material from biological origin *shells
25
Q

sediment cells

A

distinct areas of coastline separated from areas by well-defined boundaries, regarded as closed systems, vary in size

26
Q

concordant coastline

A

where the rocks lie parallel to the coast

27
Q

disconcordant

A

where the rocks lie perpendicular to the coast

28
Q

changes in sea level in last 10,000 years

A

rising an average 0,42 to 0,48 inches a year, started declining in 2010 and 2011 locked up as snow/ice

29
Q

rias

A

drowned river valleys

30
Q

fjords

A

drowned glacial valleys

31
Q

dalmatian coast

A

When the valleys are flooded by the rise in sea level, the tops of the valleys remain above the surface of the sea and appear to be a series of islands that run parallel to the coastline

32
Q

raised beaches

A

areas of former wave-cut platforms at a level higher than current sea level

33
Q

marine platform/terrace

A

formerly submerged land exposed

34
Q

effect of wave refraction on headlands

A

waves drag in shallow water, wave becomes high/steep/short, part of wave in deeper water moves faster, wave bends, low-energy wave spills into bays as most energy concentrated on headland