Chapter 15 and 16 Flashcards

mid-term review

1
Q

Aeolian system

A

wind a general part
of the circulation of the atmosphere

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2
Q

What is the aeolian system driven by? In what sorts of places?

A

Driven by solar energy. Wind is an effective agent when vegetation is
scarce (arid, glacier, coastal)

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3
Q

Where does brittle fracture occur?

A

Arid environments where breakdown is primarily brittle fracture,
regolith tends to be stony, sand and silt-grade material.

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4
Q

Sediment movement

A

Air retarded by friction with ground.
* Boundary layer condition – air is not moving at the surface
* drag velocity U*
* critical threshold velocity: threshold at which sediment moves

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5
Q

entrainment of particles by wind occurs?

A

Balance between resisting and impelling forces
-variation in atmospheric pressure can depress or raise sea level (low pressure Hurricanes sea surges)
-creates the intertidal habitat to which a range of plant and animal organisms that are adapted and which have geomorphological effects
-with each tide an influx of nutrients are brought in

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6
Q

Resisting forces

A

inertia,
* friction,
* cohesion

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7
Q

Impelling forces

A
  • drag force,
  • lift force,
  • ballistic impact
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8
Q

Waves

A

-wave action is probably the most important agent of coastal change
-wave is measured by the wavelength and height of the wave
-wind speed, duration of wind, and fetch determine wave height
-waves travel faster in open water
-waves travel slower in shallower water

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9
Q

saltation

A

process involving the movement/transportation of particles such as sand or soil by wind or water
-involves a bouncing or hopping motion where particles are lifted from the surface and then brought back down again, often to be lifted again

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10
Q

inertia

A

the tendency for objects at rest to remain at rest and for objects in motion to continue in motion unless acted upon by an outside force
-property that opposes attempts to put an object in motion or to change the magnitude or direction of its velocity

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11
Q

friction

A

the force that resists the sliding or rolling of one solid object over another

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12
Q

cohesion

A

describes particles that are the same tend to stick together

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13
Q

drag force

A

the force of wind or air resistance pushing in the opposite direction to the motion of the object (aerodynamics of a plane); friction caused by air, which opposes motion

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14
Q

lift force

A

the force exerted by moving air (wind) on a surface; acts in an upward direction in order to counter the force of gravity; a mechanical force generated by a solid object moving through a fluid

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15
Q

Erosion by wind

A
  • Removal of surface sand – leaves behind stones – desert pavement or reg
  • Wind faceted stones are called ventifacts
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16
Q

Aeolian deposition

A

process of dune formation
* Ripples
* Desert Dunes
* Coastal Dunes

17
Q

Three types of currents

A

longitudinal, transverse, surface

18
Q

nearshore dynamics

A

-waves transport sediment
-swash and backlash

19
Q

swash and backwash

A

types of wave movement that influence the structure of a beach

20
Q

swash

A

refers to waves traveling towards the beach, pushing sediment up the shoreline and contributing to coastal deposition.

21
Q

backwash

A

the movement of water back down the beach and into the ocean, which scours out the beach and carries materials away

22
Q

coastal erosion

A

if sediment removal>supply, then no beach and wave energy is directed at bedrock plus:
-salt weathering, marine organisms, water layer weathering…

23
Q

costal deposition

A

-leaving beaches(whether there is more deposition than removal of materials), sand dunes, tidal flats, and estuaries

24
Q

ripples

A

caused by the interaction of wind and water, or the physical interaction of the water with another object

25
Q

coastal dunes

A
  • An embryo foredune may form which traps further sand.
  • Positive feedback during development
  • Energy is absorbed, saltation declines and deposition occurs
  • Inland migration of the dune mass, and new dune formation
  • Vegetation stabilizes the dune
  • When disturbed by humans or animal blow out can occur
26
Q

coastal conclusion

A

-coastal processes are dominated by mechanical energy transfers at variety of temporal scales
-coasts are rapid-response systems that adapt to new equilibriums (overall younger systems)
-they are under threat from rising sea levels

27
Q

coastal system

A
  • Coasts occur where the world’s oceans and seas meet the margins of
    the land masses.
  • Estimates that 65% of world’s population lives within a few kilometers
    of the coast.
28
Q

Coastal sources of energy

A

tides and waves

29
Q

Tides

A

originate from the gravitational pull of the moon and sun in
combination with the rotational energy of the earth

  • Regular oscillations in tide level are created subject to biweekly variation can range from
    0.5-10 m
  • Variation in atmospheric pressure can depress or raise sea level (low pressure Hurricanes
    sea surges)
  • define the range of elevation in which direct wave and other marine action takes place
  • flow and ebb of tides around coastal irregularities create tidal currents
  • diurnal alternations of inundation and exposure of the intertidal zone create conditions for
    particular rock weathering processes
  • create the intertidal habitat to which a range of plant and animal organisms is adapted and which
    may have geomorphological effects
  • With each tide an influx of nutrients is supplied to intertidal organisms
30
Q

Waves

A

are created by the wind shear across the ocean (ultimately powered
by solar energy)

31
Q

What is the most important agent of coastal change?

A

wave action

32
Q

What determines wave height?

A

Wind speed, duration
of wind, and Fetch
determine

33
Q

Where do waves travel faster?

A

in open water

34
Q

Where do waves travel slower?

A

in shallow water

35
Q

What do currents do?

A

Currents (wave induced, tidal, wind-induced) transport sediments and
may entrain sediments

36
Q

salt weathering

A

a form of mechanical weathering or physical weathering of rock that occurs when salt spray from the sea gets into a crack in a rock, evaporates and crystallizes putting pressure on the surrounding rock and weakening its structure; most common in arid climates

37
Q
A