energy in coastal systems Flashcards

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1
Q

wind role (5)

A

primary source of energy

-wind speed high and uninterrupted = high wave energy
-prevailing wind determines direction waves approach and direction sediment transport
-fetch (distance blows) influences energy of waves
-influences wave formation
-can pick up sediment from coast and use it to erode other features

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2
Q

waves formation

A

primary agent in shaping the coastline

wave approaches coast and it becomes shallower
friction with seabed slows base of wave
crest continues move forward and rise
elliptical orbit
wave steepens and breaks and moves up beach as swash

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3
Q

constructive waves

A

low wave height
long wavelength
low frequency (6/min)
spill
weak backwash
move material up beach - gentle slope beach
forming berms (ridges)

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4
Q

destructive waves

A

high wave height
short wavelength
high frequency (10/min)
plunge
strong backwash
erodes material - steep beach

may project shingle up beach forming ridge called storm beach

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5
Q

negative feedback of waves

A

constructive builds beach making steeper
more destructive waves
reduces beach angle
etc

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6
Q

what is wave refraction

A

waves drag in shallower water near headland forming destructive waves which erode headland
part in deeper water moves faster so bends
wave concentrated on headland causing erosion
deposition on beach

waves pile on headland forming longshore current

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7
Q

what is a current

A

permanent or seasonal movement of surface water in oceans

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8
Q

longshore current is

A

flow of water parallel to shoreline
due to waves approaching at angle

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9
Q

rip current is

A

strong currents moving away from shoreline
as sea water piles up along coastline
flow out through breaker zone where change direction coast
dangerous

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10
Q

upwelling is

A

cold deep ocean water replacing warmer surface water
creates nutrient rich cold ocean currents

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11
Q

what is a tide

A

periodic rise and fall in sea level

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12
Q

*** how do tides form

A

moon pulls water towards it creating a high tide and therefore a compensatory bulge of the oceans surface water on the other side of earth

in between experiences low tide

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13
Q

***spring tide

A

moon sun earth all in line
produces high highs and low lows
large tidal range

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14
Q

***neap tide

A

moon and sun perpendicular to earth
low highs and low lows (10-30% lower)
small tidal range

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15
Q

what is tidal range

A

vertical difference between high tide and low tide

larger the range the greater the limit of erosion and deposition
amount of time littoral zone exposed each day increases subaerial weathering

med low range
britain high range so forms wide wave cut platforms

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16
Q

types of tidal range

A

macro= 4m+
meso = 2-4m
micro= 2m -

17
Q

what is storm surge

A

meterological conditions produce higher water levels than at high tide

north sea has depressions which cause low pressure conditions increasing sea level
1mb drop = 1cm rise
strong winds pile water up against coast causing local sea rise
north sea has funnelling

18
Q

features low energy coast

A

more deposition
spits and beaches

19
Q

features high energy coast

A

more erosion
headland/cliffs/wc platforms