coastal Flashcards

(64 cards)

1
Q

what type of system is a coast

A

it is an open system as it recieves inouts from outside systems and trasnfers outputs away from the coast into other systems. however you need to consider it as a closed system as the costal system inpacts and is impacted by the oceans.

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2
Q

what are sediment cells

A

sections of a coats wich are often borderd by prominent headlands. within these sections the movement of sediment is almost contained and the flows of sediment act in dynamic equalibrium. within sediment cells there are smaller subcells

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3
Q

what is dynamic equalibrium

A

the maintenence of a balance in a natural system, despite it being in a constant state of change. the system counteracts any changes imposedon the system in order to keep the balance

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4
Q

what is dynamic equalibrium in sediment cells

A

where input and output of sediments are in a constant state of change but remian in balance.

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5
Q

what can interupt the dynamic equalibrium

A

it can be upset in the long term by human interventions or in the short ter, by natural variations.

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6
Q

inputs def and exapmles

A

material or energy inputs. they include: marine- waves, tides, salt spray atmosphere- sun, air pressure, wind speed and direction humans- pollution, recreation, settlements, defences

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7
Q

outputs def and examples

A

material or energy outputs. e.g. ocean currents, rip tides, sediment transfer, evapouration

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8
Q

stores/sinks def and examples

A

stores and sinks of sediment and materail. e.g. beaches, sand dunes, spits, bars and tombolos, headlands adn bays, nearshore sediment, cliffs, wave cut platforms, caves, arches, stacks, stumps, salt marshes, tidal flats, offshore bands and bars

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9
Q

transfers/flows def and examples

A

the proccesses that link the inputs, outputs and stores in the coastal system. e.g windblowm sand, mass movement proccesses, long shore drift, weathering, erosion, transportation, deposition

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10
Q

energy def and exapmles

A

the power and driving force behind the transfers and flows in the system. e.g. wind, gravitational, flowing water.

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11
Q

what is the negative feedback loop

A

it lessens any change wich has occured within the system. when a system is taken out of dynamic eualibrium the negative feed back loop will balance it brining it back to dynakic equalibrium.

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12
Q

example of a negative feedback loop

A
  1. when the destructive waves from storm loose their energy excess sedimeny is deposited as an offshore bar.
  2. the bar dissipates the waves energy wich protects the beach from further erosion
  3. overtime the bar gets eroded instead of the beach
    4.once the bar has gone normal conditions ensue and the system goes back to dynamic equalibrium.
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13
Q

what is a positive feedback loop

A

this exaggarates the change making the system more unstable and taking it away from dynamic eualibrium

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14
Q

example of a positive feedback loop

A
  1. people walking over sand dunes destroys vegetation growing there and causes erosion.
  2. as the roots from the vegetation have been holding the sadn dunes together, damaging the vegetation makes the sand dunes more suspetible to erosion. this increases the rate of erosion. 3. eventually the sand dunes will be completely eroded leaving more of the beach open to erosion taking the beach further awau from its original state
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15
Q

how is a river a sediment resource

A

most of the sediment in the coastal zone is a result of an input from rivers, especially in high-rainfall enviroments where signinfiant river erosion occurs. sediment may be deposited in estuaries wich are brackish (salty) areas where rivers flow into the sea. they are important wildlife habitats. the sediment is then transported throughout the coastal system by waves, tides and currents

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16
Q

how is cliff erosion a sediment source

A

it is very important in areas with unconsolidated cliffs that are easily eroded. in some area, coastlines retreat by up to 10m per year, providing a significant sediment input. most erosion occurs during the winter months due to more frequent storms

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17
Q

how is wind a sediment resource

A

it is an energy source and can cause sand to be blown along or up a beach. sediment transport by winds may occur where there are sand dunes or in glacial and desert enviroments wich provide sediment inputs.

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18
Q

how are glaciers sediment sources

A

in some coastal systems glaciers flow directly into the ocean depostiting sediment that was stored in the ice. this occurs when glaciers calve(ice breaks off)

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19
Q

how is offshore a sediment source

A

sediment is transfered to the coastal zone when waves, tides and currents erode off shore sediment sinks such as offshore bars. the sediment is transported onto the beach, helping build up the beach. storm surges or tsunami waves may also transfer sediment into the caostal zone.

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20
Q

how is longshore drift a sediment source

A

sediment is moved along the beach due to prevaling winds which alter the direction of the waves. this allows sediment to be transported form one section of the coast to another stretch of caostline. the swash approaches the coast at an angle due to the prevaling winds, transferring sediment along the beach. the backwash pulls the sediment direvtly back down the beach. the swsh then transfers the sediment along the coastline and the proccess repeats

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21
Q

what are sediment budgets

A

they use data of inputs,outputs, stores and trasfers to sases the gains an losses of sediment within a sediment cell. in principle a system will operate in a state of dynamic equalibrium where input and outputs of sediment are equal.

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22
Q

what is the littoral zone

A

the area of land beteen the clifs or dunes on the coast and the offshore area that is beyond the influence of waves. it is therefore covered by the sea at different points in time.

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23
Q

what are the long term adn short term factors that affect the littoral zone

A

short-term: tides and storm surges
long-term: changes in sea level and human intervention

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24
Q

shore/shoreline def

A

the boundary betweeen the sea and the land

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25
offshore def
the area beyond the influence of waves
26
onshore def
the area of lanf not covered by the sea but is very close to it
27
what is the main source of energy at the coast
the main source of energy is form waves wich are formed pffshore, wich are most commnoly generated by wind or less frequently tectonic activity or underwater landslides causing tsunami waves
28
how do waves form
wind moves across the surface of the water, causing frictional drag wich creates small ripples and waves. this leads to a circular orbital motion of water particles in the ocean. as the seadbed becomes shallower towards the coastline, the orbit of the water particles become more elliptical, leading to more horizontal movement of the waves. the wace height increases, but the wave length and ave velocity bith decrease. this causes water to back up from behind the wave until the wave breaks and surges up the beach
29
how does wind strength affect wave energy
wind is air that moves from an area of high pressure to an area of low pressure. the different pressures are cuased by variation in surface heating by the sun. the larger the difference in pressure between the toe areas the stonger the winds. as winds casue waves, stronger winds also mean stronger waves.
30
how does wind duration affect wave energy
if the wind is active for longrt periods of time, then the energy of the waves will build up and increase.
31
how does the size of the fetch affect wave energy
the fetch is the distance over wich the wind blows and the larger it is, the more powerful the waves will be. it could also be thought of as distance to the nearest land mass in a particular direction
32
what is the formation of a constructive
it is formed by weather sytems that operate in the open ocean
33
what is the wavelength on a constructive wave
long wavelength
34
what is the frequency of cinstructive waves
6-9 per minute
35
what are the characteristics of constructive waves
low waves, wich surge up the beach
36
what are the swash characteristics of constuctive waves
strong swash, weak back wash
37
what effect do constructive waves have on the beach
occurs on gently sloped beaches
38
how are destrcutive waves formed
localised storm events with stronger winds operating closer to the coast
39
what is the wave lenth of a destructive wave
short wavelength
40
what is the frequency of destructive waves
11-16 per minute
41
what are the characteristics of a destructive wave
high waves, wich plunge onto the beach
42
what are destructive wave swash characteristics
weak swash, strong backwash
43
what are destructive waves effect on the beach
occurs n steeply sloped beaches
44
what is the negative feedback proccess of beaches and waves
constructive waves cause depositionn, wich leads to the beach profile becoming steeper. steep beaches favour the formation of destructive waves. the destructive waves erode the beach reducing the profile and leading to the formation of construtive waves.
45
how does the beach profile change throughout the year
constructive waves occur more in sumer when there are fewer storms meaning the beach profileis genteler and steeper during the winter months when destructive waves are more common. this leads to the state of dynamic.
46
how are tides formed
gravity pulls the sun or moon and changes the water levels of the seas and oceans.
47
what is tidal range
the difference in height between tides and it tends to be largest in channels such as river esturies.
48
what is a spring tide
its when the highest and lowest tide occur. this happens when the sun and the moon are in aligment. both of their gravitational forces combine to effectivly pull teh oceans towards them to cause the highest tides. on the other side of the planet this creates the lowest possible low tide.
49
what is a neap tide
its when the lowest high tide and highest low tide occur. this happens when the sun and moon are perpendicular to eachother.both their gravitational forces act against eachother, so the overall pull is minimised at high tide, but therefore creates a higher low tide.
50
what are rip currents
powerful underwater currents occuring in areas close to the shoreline on beaches when plunging waves cause a buildup of water at the top of the beach.
51
how are rip currents formed
the backwash is forced under the surface due to resistsnve frombreaking waves, forming an underwater curent. this flows away from the shore more quickly due to resistance from breaking waves, forming an underwater current. this flows away from the shoremore quickly due to beach features, suchas a gip in a sandbar.
52
what are riptides
they are an energy source in coastal enviroments and can lead to outputs of of sediment from the beach area. they occur when the tide pulls warer througha small area such as a bay or lagoon.
53
where do high energy coastlines occur and their factors
they occur is areas where there is a large fetch as there are more powerful waves. they typically have rocky headlands and landforms and fairly frequent destructive waves. as a result the coastlinesare often eroding as the the rate of erosion exeeds the rate of deposition.
54
where do lowenergy coastlines occur and their factors
they occur is sheltered areas where less powerful constructive waves prevail and as a result these areoften fairlt sandy areas. there are landforms of deposition as the rate of deposition exeeds the rate of erosion.
55
what is waves refraction
the process hwere waves turn and lose energy around a headland on uneven coastlines. the wave energy is focused on the headlands, creating erosive features in these areas. the energy is dissipated in bays leading to the formation of features associated with lower energy enviroments such as beaches.
56
negative feedback process of headlands and bays
different rock strengths lead to the formation of headlands where resitant rocks and bays where unconsolidated rocks and clays are dominant. this then increases theforces of erosionon the headlands and reduced erosion on the bays as wave refraction dissipates wave energy and a beach protects the coastline behind. eventually the headland is worn away wich then increases erosion withinthe bays. this wouldlead to dynamic equlibrium if conditions stayed constan.
57
erosion as a marine proccess def
a collaborative proccess wich invloves the removal of sediment from a coastling by difefrent types of erosion not one type acting by itslef.
58
corrasion def
sandand pebbles are picked uo by the sea from an offshore sediment sock or temporal store and hurled agaisnt thecliffs at high tide, causing the cliffs to be eroded
59
abrasion def
the proccess where sediment is moved along the shoreline, causing it to be worn down overtime.
60
attrition def
wave action cause rocks and pebbles to hit against eachother, wearing eachother dowm and so becoming round and eventually smaller. its an erosive proccess within the coastal enviroment but has little to no effect of the erosion of the coastline.
61
hydraulic action def
as waves crash onto a cliff face, air is forced into cracks, joints and faults within the rock. the high presure causes the cracks to force apart and widen when the wave retreats and the air expands. overtime this causes the rock to fracture.
62
cavitation def
bubbles found within the warer may implode under the high pressure creating tiny jets of water that overtime erode the rock.
63
corrosion (solution) def
the midily acidic seawater can cause alkaline rock such as linestone to be eroded and is very similar to the process of carbonation weathering.
64
wave quarrying def
when breaking waves that hit the cliff face exert a pressure upto 30 tonnes per meter squared. it is very similat to hydraulic action but acts with significantly more pressure to directly pull away from a cliff face or remove smaller weathered fragments. the force of the breaking wave hammers the rock surface, shaking and weekening it and leaving it open to hydraluc action and abrasion.