Estuaries and coasts Flashcards

1
Q

What is an estuary?

A

A portion of the ocean:
- Diluted by freshwater input
- Semi-isolated by land

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2
Q

What are the 3 key aspects of an estuary?

A
  • Geometry
  • Rate of freshwater input
  • Strength of tidal flows
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3
Q

What happens when fresh and salt water meet?

A

‘Lock-exchange experiment’

  • Two layer flow
    → → less dense fresh water outflow above more dense salt water inflow (density-driven circulation)
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4
Q

What is circulation modified by?

A
  • Mixing between fresh and salt water
  • Tidal movement of the salt water in and out of estuary
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5
Q

What are the types of estuary?

A
  • Salt wedge
  • Partially-mixed
  • Well-mixed
  • Fjord
  • Inverse (?)
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6
Q

What occurs in salt wedge estuaries?

A
  1. Fresh water flows out at surface (net seawards flow is almost all fresh water) from 0 ppt to 15 ppt
  2. Salt water intrudes at depth, the salt wedge moves in and out of estuary with tide
  3. Salt water is held back by fresh water → sharply tilted interface
  4. Fresh water erodes saltwater → one-way mixing (entrainment
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7
Q

What occurs in partially-mixed estuaries?

A
  1. Surface flow exceeds freshwater flow
  2. Salt inflow is due to advection and diffusion
  3. density contours tilted
  • Increased tidal mixing with reduced river flow mixes salt water into surface layer
  • Rapid exchange of water
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8
Q

What occurs in well-mixed estuaries?

A
  1. Slow net seawards flow at all depths
  2. Salinity becomes uniform with depth
  3. Little or no inward transfer of seawater

Even greater tidal mixing with reduced river flow leads to well mixed estuary

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9
Q

What occurs in Fjord estuaries?

A
  1. River flow remains at surface and moves seaward with little mixing
  2. Little inflow of water at depth (still acts as a barrier)
  3. Deeper water may stagnate
  • Deep basin with entrance sill
  • Moderate river flow and little tide
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10
Q

What are the features of an inverse estuary?

A
  • Salinity increases up estuary
  • Surface inflow of seawater
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11
Q

What are inverse estuaries not strictly an estuary?
Why

A

As in hot, dry regions evaporation may dominate over precipitation and river inout

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12
Q

What is true of calm/swell/summer beach profile changes?

A
  • Low waves → weak undertow
  • Accretion dominant → berm
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13
Q

What is true of energetic/storm/winter beach profile changes?

A
  • High waves → strong undertow
  • Erosion dominant → offshore sandbar
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14
Q

How are coastal dunes formed?

A

Formed from wind blown sand

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15
Q

What do coastal dunes feature?

A
  • Primary dune ridge
  • Secondary dune ridge
  • Foredunes
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16
Q

What is true of coastal dunes?

A
  • Vegetation is important as this stabilises the dunes, and the absence may lead to blow-outs
  • They are susceptible to wave attacks
17
Q

What is aeolian sand transport? (Coastal dunes)

A

It is the first process of coastal dune formation and involves the movement and weathering of sand particles behind and parallel to the shoreline.

18
Q

What are barrier islands?

A
  • Large sand deposits separated from mainland by estuary, bay or lagoon
    —- Abundant sand supply
    —– Low seafloor slope
19
Q

How are barrier islands formed?

A
  • Submergence of coastal sand ridge
  • Segmentation of sand pit
  • Emergence of longshore sand bar
20
Q

What is true of clipped coasts?

A
  • Changes often associated with spectacular failure
    —– Wave erosion at cliff base
    —– Land processes (groundwater)
21
Q

How are delta coasts formed?

A

Built for river sediments

22
Q

What are the 3 zones of delta coasts?

A

Delta plain, delta front and prodelta