EAE3311 Week 9 Flashcards

1
Q

<p><span>Definition</span></p>

<p><strong><span>The shore</span></strong></p>

A

<p><span>The zone that lies between the lowest tide level (LAT) and the highest elevation on land that is affected by storm waves.</span></p>

<div>Width ranges from a few meters to hundreds of meters (tidal range, storm surge).</div>

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2
Q

<p><span>Definition</span></p>

<p><strong><span>The coast</span></strong></p>

A

<p><span>Extends inland from the shore as far as ocean related features can be found (this can be many 10s of km)</span></p>

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3
Q

<p><span>Definition</span></p>

<p><strong><span>The coastline</span></strong></p>

A

<p><span>Marks the boundary between the shore and the coast<br></br>(the landward limit of where ocean water reaches)</span></p>

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4
Q

<p><span>Definition</span></p>

<p><strong><span>Coastal areas</span></strong></p>

A

<p><span>A definition used in social sciences, population studies and policy making.<br></br>Usually defined as within 100 km of the coastline</span></p>

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5
Q

<p><span>Definition</span></p>

<p><strong><span>Low elevation coastal zone</span></strong></p>

A

<p><span><10 m elevation in the coastal area</span></p>

<p><span>EAE3311 9ae</span></p>

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6
Q

<p><strong><span>How is population distributed from the coast?</span></strong></p>

<p>2 points.</p>

A

<p><span>Presently, 40% of the world’s population lives with 100 km of the coast</span></p>

<ul> <li>Access to ocean navigation, coastal fisheries, tourism and recreation.</li> <li>Vulnerability to sea-level rise and other coastal hazards such as storm surges.</li></ul>

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7
Q

<p><span>Describe</span></p>

<p><strong><span>Sea Level</span></strong></p>

A

<p><span>The interface between the sea and the atmosphere</span></p>

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8
Q

<p><span>Describe</span></p>

<p><strong><span>Landmass at the coast</span></strong></p>

A

<p><span>The interface between the land and the atmosphere</span></p>

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9
Q

<p><strong><span>What is the relationship between Sea Level and Landmass at the coast?</span></strong></p>

A

<p><span>Both move independently of each other relative to the centre of the Earth (Geoid)</span></p>

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10
Q

<p><span>Definition</span></p>

<p><strong><span>RSL</span></strong></p>

A

<p><span>Relative Sea Level</span></p>

<div>RSL = SL - R</div>

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11
Q

<p><span>Definition</span></p>

<p><strong><span>SL</span></strong></p>

A

<p><span>Sea Level</span></p>

<div>(mainly to do with the growth and decay of ice mass)</div>

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12
Q

<p><span>Definition</span></p>

<p><strong><span>R</span></strong></p>

A

<p><span>land motion</span></p>

<div>R>0 uplift</div>

<div>R<0 subsidence</div>

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13
Q

<p><span>Describe</span></p>

<p><strong><span>Waves in the coastal zone</span></strong></p>

<p>4 points.</p>

A

<p><span>Waves are all important in the coastal zone</span></p>

<ul> <li>Waves have equal amounts of kinetic and potential energy</li> <ul> <li>Potential energy (the energy acquired by resisting gravity)</li> <li>Kinetic energy (the energy acquired by a mass in motion)</li> </ul> <li>Energy carried by the wave is proportional to the height and speed of the wave</li></ul>

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14
Q

<p><span>Describe</span></p>

<p><strong><span>The flux of wave energy (Wave Power)</span></strong></p>

A

<p><span>Each metre of wave crest delivers 36 kW of power</span></p>

<div>P(kW/m)=0.5 Hₛ² Tₑ</div>

<div></div>

<div>NB Formula applies to 'deep water'</div>

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15
Q

<p><span>Definition</span></p>

<p><strong><span>Deep Water</span></strong></p>

A

<p><span>Depth > ½ Wave Length</span></p>

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16
Q

<p><strong><span>The flux of wave energy (Wave Power) - Shallow Water</span></strong></p>

<p>2 points.</p>

A

<div>1/2 </div>

<div></div>

<ul> <li>The shallower the water, the less power is left in the wave. </li> <li>More energy arriving at the cliff when the tide is high</li></ul>

<div></div>

<div></div>

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17
Q

<p><span>Describe</span></p>

<p><strong><span>The dynamics of coastal systems: where is the work done </span></strong></p>

<p>6 points.</p>

A

<p><span>Wave energy is deposited where the sea meets the land</span></p>

<ul> <li>As the waves arrive to shore they transform and break when they get too steep.</li> <li>The plunging waves thrust water onto the shore-face (swash) which recedes as backwash</li> <li>High shoreward speed, 'wave setup' of water above SWL</li> <li>Conservation of Mass = runs back down</li> <ul> <li>Undertow</li> <li>Rip Currents (jets that intercept the breaker line)</li> </ul></ul>

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18
Q

<p><span>Describe</span></p>

<p><strong><span>Constructive Waves vs Destructive Waves</span></strong></p>

<div>A very simplified way of looking at this</div>

A

<ul><li>Under calm wave conditions, sand moves onshore and the beach builds into a broad feature with a well-developed berm. Fair weather waves tend to be swells of low amplitude and long period. </li><li>Strong asymmetry in the associated bottom wave surge with the landward stroke beneath the wave crest (swash) being significantly more intense than the seaward stroke beneath the trough (backwash). </li><li>Differential velocity moves sand upslope and onshore (except in zones of rip currents).</li></ul>

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19
Q

<p><span>Describe</span></p>

<p><strong><span>Constructive waves </span></strong></p>

<p>4 points.</p>

A

<ul> <li>Low amplitude (height)</li> <li>Long period: time for swash to run up the beach without being interrupted by backwash</li> <li>Swash >> Backwash</li> <li>Erosion leaves behind larger grains</li></ul>

<div><strong>Opposite for Destructive waves</strong></div>

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20
Q

<p><span>The dynamics of coastal systems: where is the work done</span></p>

<p><strong><span>Rocky Shores </span></strong></p>

<p>3 points.</p>

A

<ul><li>Active margins </li><li>Rocks uplifted faster than sea level </li><li>Result = rocky cliffs interspersed with pockets of sand</li></ul>

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21
Q

<p><span>The dynamics of coastal systems: where is the work done</span></p>

<p><strong><span>Sandy Shores </span></strong></p>

<p>4 points.</p>

A

<ul> <li>Passive margins</li> <li>Sea rises faster than the land surface</li> <li>Sand is spread out over the littoral zone through a range of processes</li> <li>30% of the world's ice free shorelines</li></ul>

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22
Q

<p><span>Key points</span></p>

<p><strong><span>Rocky coastline</span></strong></p>

<p>6 points.</p>

A

<ul> <li>Wave power leads to rock erosion</li> <ul> <li>Quarrying</li> <li>Plucking of rocks</li> <li>If the wave carries sand, abrasion</li> </ul> <li>A rock experiencing a typical ocean swell of 10-20 s experiences >1 million impacts/ year</li> <li>Impact can be measured seismically, cliff sways a few microns with every passing wave</li></ul>

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23
Q

<p><span>Key points</span></p>

<p><strong><span>Beaches</span></strong></p>

<p>4 points.</p>

A

<ul> <li>The beach is a 3D structure (practically a loose pile of sand in a high energy environment) that moves both in a cross shore and an along shore direction.</li> <li>When the material comes from the erosion of beach cliffs or nearby coastal mountains, beaches are composed of mineral particles that can be relatively coarse.</li> <li>When the material comes primarily from rivers that drain lowland areas, the grains are very fine (e.g. clay and silt) and mud flats develop.</li> <li>Some beaches have a significant biological component.</li></ul>

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24
Q

<p><span>Key points</span></p>

<p><strong><span>Beaches - movement</span></strong></p>

<p>4 points.</p>

A

<ul> <li>Regardless of the composition, these material are in transit along the shoreline ('rivers of sand').</li> <li>The movement of sand is both</li> <ul> <li>parallel (alongshore) </li> </ul></ul>

<div>and</div>

<ul> <ul> <li>perpendicular (cross shore) to the shoreline</li> </ul></ul>

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25
Q

<p><strong><span>How can we measure longshore drift?</span></strong></p>

A

<p><span>Long term longshore drift rates can be measured as the accumulation of sediment behind natural or human-made structures </span></p>

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26
Q

<p><span>Key points</span></p>

<p><strong><span>Beach morphology</span></strong></p>

<p>3 points.</p>

A

<ul><li>Self-organisation vs. chaos </li><li>Landforms can have spatial order at a range of scales derived from internal forcings and dynamics (fractal pattern formation).</li><li>But coastal systems are non-linear dissipative systems where wind, currents and waves deposit energy (multiple elements with non-linear interactions)</li></ul>

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