Aeolian processes: incl. erosion, deposition, transportation Flashcards

1
Q

what planets could have aeolian activity

A

all terrestrial planets with dynamic atmospheres- mars, venus, earth

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2
Q

why is aeolian erosion and transport especially effective in deserts

A

sediment largely loose in sandy deserts and not held by vegetation due to moisture deficit, the carried sand makes the wind more erosive

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3
Q

what is the kármán line

A

the line approx 100km above the earths surface that delineates the boundary of atmosphere and space

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4
Q

what does it mean to say the atmosphere is in hydrostatic equilibrium

A

pressure is exerted in all directions, making it relatively stable

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5
Q

layers of the atmosphere

A

thermosphere, mesosphere, stratosphere, troposphere

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6
Q

describe laminar flow

A

thin sheets of moving air over one another, little mixing of layers with the surface air being stationary

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7
Q

describe turbulent flow

A

mixing between layers, gusts and eddies, surface layer is stationary

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8
Q

what causes turbulent wind flow

A

variations in surface topography or variable surface heating

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9
Q

which type of air flow can entrain sand more easily

A

turbulent

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10
Q

what is the reynolds number

A

it distinguishes between laminar and turbulent flow

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11
Q

what wind has the highest velocity in the troposphere

A

jet stream

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12
Q

what is the boundary layer

A

the layer roughly 300m in altitude in which all exchanges between surface and atmosphere take place

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13
Q

describe the wind conditions of the boundary layer

A

turbulent flow, slower due to friction, dust storms will fill up within the boundary layer

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14
Q

what is the roughness layer

A

2-5cm over grass or 2-5 m in forests, almost still flow

can be determined by plant height and flexibility

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15
Q

what is the roughness length

A

height where the wind is effectively 0m per second

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16
Q

3 forces that work together to entrain sediment in the wind

A

gravity- keep grain at surface, drag- moves grain along ground, lift- shear stress

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17
Q

4 methods of aeolian sediment transport

A

suspension, creep, reptation, saltation

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18
Q

describe creep

A

grain remains in contact w surface most of the time, coarser grains,

19
Q

describe reptation

A

hopping motion, transitional between creep and saltation, hit other grains and cause them to bounce forward

20
Q

describe saltation

A

jumping motion, 35 degree angle, parabolic pathway, 2-4cm height, dominant transport method

21
Q

5 factors influencing sediment entrainment in aeolian systems

A
sediment size
surface vegetation
surface crusting
surface moisture
surface slope
22
Q

what is fluid threshold velocity

A

min wind speed to initiate grain movement by wind force alone

23
Q

what is impact threshold

A

min wind speed needed to initiate particle movement as a result of reptation

24
Q

what bacteria can create organic crusts

A

cyanobacteria

25
Q

what moisture content is the threshold to inhibit sediment transport

A

2-5%

26
Q

what is the effect of fog on entrainment

A

can reduce ability of wind to cause entrainment

27
Q

name the 2 sides of a dune

A

windward slope and slip face

28
Q

which dune side is steepest

A

slip face

29
Q

which slope is easier to erode

A

downslope- decreased critical threshold

30
Q

impact of surface veg on entrainment

A

surface roughness length due to plants slows velocity- plant height and flexibility

31
Q

what 2 main factors make up sediment movement

A

erosivity (power of wind) and erodibility (grain characteristics holding particles in place)

32
Q

what is deflation

A

aeolian erosion: wind causes the lifting and transport of lighter particles from dry soil

33
Q

what feature can show the predominant wind direction of the past or present

A

lunettes: dust plume deposits formed from the wind moving material away from lake hollows

34
Q

formation of desert pavements

A

wind picks up finer materials through deflation and leaves behind lag deposit-> stony pavement becomes a protective layer

35
Q

3 controls on wind erosion

A

susceptible surfaces, sufficient wind energy, removal from site of eroded material

36
Q

what is abrasion

A

erosion by suspended sand particles (transfer of kinetic energy)

37
Q

what is a ventifact

A

a rock sculptd by wind-borne particles (worn, faceted, cut or polished by these particles)

38
Q

what is the facet of a ventifact

A

a curved or flat surface cut by the wind into a ventifact

39
Q

what is a keel on a ventifact

A

sharp edge or ridge between the lee and windward side of a ventifact

40
Q

what is the difference between flutes and grooves

A

grooves open through while flutes are closed at each end

41
Q

when did most abrasion on rocks seen today occur

A

last glacial maximum with v high winds and lots of dust

42
Q

what are pedestal rocks

A

shaped like a mushroom, undercut by wind abrasion/ enhanced chemical weathering at the base

43
Q

what are yardangs

A

long ridges of resistant rock jutting out of the landscape due to the erosion of less resistant rock first
micro-yardangs can form on top
meso-yardangs are smaller and more assymmetrical, have a flat steep side and sloping downwind side