stability and cooling/heating

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74 Terms

1
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How is the troposphere heated

The troposphere is heated from the Earth by terrestrial radiation and conduction.

2
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What is terrestrial radiation

The Earth absorbs the sun’s rays, heats up, and emits its own radiation.

3
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Which gases absorb terrestrial radiation

CO₂ and H₂O vapour.

4
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Does terrestrial heating increase or decrease with altitude

It decreases as radiation energy lessens.

5
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Which heats faster: land or water

Land heats quicker.

6
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Which cools faster: land or water

Land cools quicker.

7
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What is conduction

Heat transfer through direct contact.

8
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How does conduction heat the air

Air in contact with the surface heats or cools depending on the surface temperature.

9
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How deep into the troposphere does conduction affect

The first 4000 feet.

10
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How is heat distributed vertically through the troposphere

By convection, turbulent mixing, release of latent heat, compression, and advection.

11
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What is convection

Air warmed by radiation or conduction becomes less dense and rises.

12
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What causes air to stop rising in convection

When it cools, becomes denser, and sinks.

13
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Does convection occur on small scales, large scales, or both

Both.

14
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What is turbulent mixing

Wind blowing over rough terrain produces eddies that mix air vertically.

15
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What is an eddy

A circular motion of air moving contrary to the main flow.

16
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What causes latent heat release

Condensation occurring after water vapour reaches its dewpoint.

17
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What does evaporation require

Heat absorption.

18
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What does condensation release

Latent heat into the atmosphere.

19
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How is heat transported upward by latent heat

Water vapour carries heat aloft before releasing it during condensation.

20
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What is compression in the atmosphere

Subsiding air enters higher pressure and warms as it compresses.

21
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What is subsidence

Descending air from higher altitudes.

22
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Why does compressional heating occur

Same amount of air molecules in less space increases temperature.

23
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What is advection

Horizontal transport of atmospheric properties such as air and moisture.

24
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When does advectional warming occur

When cool air moves over a warmer surface.

25
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How is the atmosphere cooled

Temperature decreases with height; nighttime radiational cooling; conduction cooling the lower 4000 feet.

26
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What is the Environmental Lapse Rate (ELR)

The actual temperature decrease with altitude at a given time and place.

27
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What is the average ELR

1.98°C per 1000 feet.

28
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Why does the atmosphere cool at night

More radiation is emitted than absorbed.

29
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What is expansional cooling

As air rises, pressure drops, air expands, and temperature decreases.

30
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Why does rising air expand

Air pressure decreases with altitude.

31
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Define adiabatic. Occurring without gain or loss of heat.

32
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What happens to a gas compressed adiabatically

Its pressure and temperature increase without heat exchange.

33
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What happens to a gas expanded adiabatically

Its pressure and temperature decrease without heat exchange.

34
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What is adiabatic heating

Heating due to compression of descending air.

35
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What is adiabatic cooling

Cooling due to expansion of rising air.

36
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What is the Dry Adiabatic Lapse Rate (DALR)

3°C per 1000 feet.

37
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When does air cool at the DALR

When it is unsaturated.

38
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What happens when rising air reaches dewpoint

Condensation begins.

39
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What effect does condensation have on temperature

Releases latent heat, reducing the rate of cooling.

40
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What is the Saturated Adiabatic Lapse Rate (SALR)

1.5°C per 1000 feet.

41
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Why is SALR lower than DALR

Latent heat released during condensation warms the air.

42
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Name the six adiabatic cooling methods. Orographic lift, upslope lift, frontal lift, mechanical turbulence, convection, convergence.

43
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What is orographic lift

Air forced upward over a mountain.

44
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What is upslope lift

Air cools as it is lifted up gradually rising terrain.

45
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What is frontal lift

Warm air being forced upward along a front.

46
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How does warm air rise along a warm front

It slides up over retreating cold air.

47
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How does warm air rise along a cold front

Cold advancing air undercuts warm air, forcing it upward.

48
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How does mechanical turbulence cause cooling

Air is pushed upward by surface friction and expands/cools.

49
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Why does convection cause cooling

Warmer surface areas cause buoyant rising air that expands/cools.

50
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What is convergence

Surface winds flowing inward toward a low pressure center and rising.

51
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What is stability

The tendency of an object to return to its original position if displaced.

52
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What is stable air

Air that resists vertical motion.

53
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What is unstable air

Air that promotes vertical motion.

54
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What is neutral air

Air that neither resists nor promotes vertical motion.

55
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What determines whether air rises or sinks

Its buoyancy compared to the surrounding air.

56
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When is air more buoyant

When it is warmer (less dense) than the surrounding air.

57
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When does unstable air stop rising

When it becomes the same temperature as surrounding air.

58
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How do you determine atmospheric stability

Compare the lapse rate of rising air to the lapse rate of surrounding air.

59
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What is the surrounding (non-rising) air lapse rate

2°C per 1000 feet (ICAO standard lapse rate).

60
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What lapse rates must be compared for stability

ELR vs DALR or SALR.

61
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If ELR is greater than DALR, is the air stable or unstable

Unstable. (Slide does not answer; aviation rule provided.)

62
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If ELR is less than SALR, is the air stable or unstable

Stable. (Aviation answer added.)

63
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If ELR is between DALR and SALR, what type of stability

Conditionally unstable. (Added question.)

64
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What is the albedo effect

Darker surfaces absorb more solar radiation.

65
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What type of surface has highest albedo

Fresh snow.

66
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What type of surface has lowest albedo

Asphalt or dark soil.

67
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What happens when winds converge at the center of a low

Air is forced upward, cools, and expands.

68
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Which cooling method is responsible for most cloud formation

Adiabatic cooling.

69
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Which lifting method is most common on windy days over rough terrain

Mechanical turbulence.

70
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Which lifting method generates lenticular clouds

Orographic lift. (Added aviation knowledge)

71
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What does convection typically create

Cumulus clouds.

72
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Why does rising air cool

Decreasing pressure causes expansion.

73
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Why does descending air warm

Increasing pressure causes compression.

74
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What determines cloud base height

Temperature–dewpoint spread. (Added aviation knowledge)