2.1. Wave, marine and sub-aerial processes Flashcards

1
Q

Define wave

A
  • Waves are oscillation of the water surface
  • Water does not move forward
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2
Q

Define wave height/amplitude

A

The distance between the trough and the crest Indication of wave energy

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3
Q

Define wavelength

A

The distance between successive crests or troughs

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4
Q

Define wave frequency

A

The number of waves per minute

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5
Q

2 Factors affecting the formation and size of a wave

A
  1. Wind velocity
  2. Depth of water Fetch - the distance of open water the wave travels over
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6
Q

What are the coastal zones? (3)

A
  1. Upper beach/backshore - backed by cliffs or sand dunes
  2. Foreshore - periodically exposed by tides
  3. Offshore - covered by water
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7
Q

Define wave orbit

A
  • The shape of the wave. Varies between circular and elliptical. The orbit diameter decreases with depth (roughly equal to wavelength)
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8
Q

Define wave base

A

When the orbit diameter decreases to a point there is no further movement related to wind energy

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9
Q

Define swell waves

A

Waves that are characterised by lower height and longer wavelength

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10
Q

Define wave breaker

A

Occurs when waves move further onshore, friction slows down the wave advance causing the shortening of wave

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11
Q

What are the 3 main types of breaker?

A
  1. Spilling breakers
  2. Plunging breakers
  3. Surging breakers
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12
Q

What are spilling breakers?

A
  • Are associated with gentle beach gradients and steep waves are characterised by gradual peaking of the wave until the crest becomes unstable => gentle pilling forward of the crest
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13
Q

What are plunging breakers?

A
  • Tend to occur on steeper beaches than spilling breakers with waves of intermediate steepness distinguished by the shore ward face of the wave becoming vertical, curling over and plunging forward.
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14
Q

What are surging breakers?

A
  • Found on steep beaches with low steepness waves, the front face and crest of the wave remain relatively smooth a large proportion of the wave energy is reflected at the beach
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15
Q

Define swash, backwash

A
  1. Swash: forward movement of water up the beach
  2. Backwash: backward movement of water down the beach
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16
Q

Define constructive waves/swell waves (6)

A
  • Swash is greater than backwash
  • Large fetch
  • Long wave length
  • Low height
  • Found on low gradient beaches, low energy waves which deposit materials
  • Associated with spilling breakers
17
Q

Define destructive waves/stom waves (6)

A
  • Backwash is greater than swash
  • Short fetch
  • Short wave length
  • High waves and frequency
  • Steeply sloping beaches
  • High energy waves which erodes
18
Q

Define tide

A
  • regular movements in the sea’s surface, caused by the gravitational pull of the moon and sun on the oceans
  • Low spring tides occur just after a new moon
  • Hgh spring tides occur after a full moon
19
Q

Define tidal range

A

The difference between high and low tide

20
Q

3 types of rides coastal areas can be classified into?

A
  1. Microtidal
  2. Mesotida: 2-4m
  3. Macrotidal - > 4m
21
Q

Define storm surges ( bão lao tới/ bão dâng lên)

A
  • Changes in the sea level caused by intense low pressure systems and high wind speeds for every drop in air pressure of 10mb sea water is raised 10 cm
22
Q

Define wave refraction

A
  • Is the change in speed and distortion of wave
  • Waves are refracted and energy is concentrated around headlands and more dispersed (phân tán) along beaches located in:
  • Bays headland - converging waves, deeper waters (erosion)
  • Bay - diverging waves, shallower waters (deposition)
23
Q

4 types of erosion

A
  1. Hydraulic action: water breaks against cliff face, air trapped in cracks and joints => cavitation
  2. Corrasion/Abrasion: process whereby breaking wave can hurl pebbles and shingle against a coast and thus abrading it
  3. Attrition
  4. Solution
24
Q

5 Mass movements occur in coasts

A
  1. Salt weathering
  2. Freeze thaw weathering
  3. Biological weathering
  4. Solution weathering
  5. Slaking ( sự dập tắp )
25
Salt weathering
the process by which **sodium** and **magnesium** compounds **expand in joints** and **cracks =\> weakening** rock structures
26
Freeze-thaw weathering
The process whereby **water freezes,** **expands** and degrades (giảm bớt) jointed rocks
27
Biological weathering
Carried out by **molluscs**, s**ponges** and **sea urchins** that burrow (đào bới)
28
Solution weathering
The chemical weathering of **calcium** by **acidic** water
29
Slaking ( làm dãn ra)
Materials disintegrate (phân tán) when exposed to water
30
2 Energy factors affecting the rate of erosion
1. **Waves -** **wave steepness** (steep destructive waves have more erosive power) and **wave breaking point** (where wave break at cliff base that cause maximum erosion) 2. **Tides Currents Winds** - **onshore wind**s erode **fine beach materia**l, **offshore winds** erode **dunes**
31
4 Material factors affecting the rate of erosion
1. Sediment supply - continual supply -\> **abrasion. oversupply can protect the coast** 2. Beach/rock platform width - absorb wave energy 3. Rock resistance 4. Rock structure - well jointed
32
Shore geometry factors affecting rate of erosion (3)
1. **Offshore topography** - **steep seabased** creates **higher** and **steeper waves**; l**ongshore bars** cause **waves to break offshore** and l**ose energy** 2. **Orientation of coast** - **headlands** with **vertical cliffs** tend to **concentrate wave energ**y by refraction 3. **Direction of fetch** - longer **the fetc**, greater potential for erosion
33
How is the sediment transport categorised? (2)
2 modes: 1. **Bedload** - **grains transported** by bedload are moved t**hrough continuous traction** or **discontinuous saltation** 2. **Suspended load** - grains are **carried by turbulent flow** and **held up by wate**r. **Strong currents**
34
Define sediment cells (2)
1. A section of the **coastal zone** here the **sediment** in the **nearshore zone** is moved by **longshore drift** 2. **Sediment cells** have **clear boundarie**s to define them such as headlands
35
4 Inputs to sediment cell
* **Cliff** erosion * **offshore** bars * **river** sediment * **sand dunes** eroding -\> depositional feature *e.g. beach*
36
Transportation in a sediment cell (4)
1. **Longshore** drift 2. **saltation** 3. **traction** 4. **suspension**
37
Stores of a sediment cell (1-3) (2-1)
1. **temporary** features - beaches, dunes and spits 2. bars **permanent** stores - estuary
38
Notes about sediment cell
* In reality it is **unlikely that sediment cells are fully closed**. With **variations** in **wind directions** and **tidal currents**, it is **inevitable** that some **sediment is transferred between cells**
39
Define **dynamic equilibrium** (2)
1. The concept states that any system (sediment cell for example) is the **result of the inputs** and **processes** that **operate within it.** 2. **Change to one of the input**s will cause a **knock on effect** on t**he process** and resulting a c**hange** in **the landforms**. *e.g. increase in sediment =\> **beach protetion** =\> **stabilisation** of cliffs*