Atmosphere Theory Flashcards

1
Q

What is humidity?

Compare humidity at a given temperature at 5,000 feet with that at sea level:

A

Measurement of water vapor in air relative to dewpoint.

For a constant temperature, but a difference in air pressure, the vapor pressure (absolute humidity) at 5,000 feet will be lower than at the surface, simply because the air pressure is lower (the partial pressure of all molecules would be less). However, the saturation vapor pressure (which is dependent solely on temperature) at 5,000 feet will be the same as at the surface, if the temperature at the surface and 5,000 feet is the same.
Relative humidity is the ratio of vapor pressure to saturation vapor pressure. The relative humidity would be less at 5,000 feet than at the surface, because the vapor pressure is less at 5,000 feet

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2
Q

What is the composition of the earth’s atmosphere?

A

78% Nitrogen
21% Oxygen
1% Other

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3
Q

Static Pressure results from:

A

The static pressure of the air at any altitude results from the mass of air supported above that level.

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4
Q

At 40,000 feet what is the percentage of:
1. Static Pressure
2. Density
Compared to standard sea level?

A
  1. 19% (20%) Static Pressure
  2. 25% Density
    Of the sea level volume.
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5
Q

What is the standard sea level temperature, pressure and density?

A

15C
14.7psi / 29.92 in.Hg
1.225 kg/m3 or 0.002378 slugs per cubic foot
(A slug (sl) is an Imperial unit of mass that accelerates by one foot (per second) (per second) (1 ft/sec²) upon force of one pound-force (1 lbf))

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6
Q

What is the most important property when studying aerodynamics? (Static Pressure, Temperature, Density, Viscosity, etc.)

A

Density (density altitude and temperature)

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7
Q

Define the density of the air:

A

The mass of air per cubic foot and a direct measure of the quantity of matter in each cubic foot. Decreases with an increase in altitude.

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8
Q

How much does air weigh at a standard sea level condition?

A

0.0765 pounds per cubic foot (3/4 of 1/10 of a pound)

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9
Q

Define viscosity:

A

Viscosity is a measure of resistance to flow. (Thickness)

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10
Q

Why are the viscosity of gases unusual?

A

Because the viscosity is generally a function of temperature alone and an INCREASE in temperature increases the viscosity. (Low viscosity flows easily because its molecular makeup results in very little friction when it is in motion. Higher temperature increases the frequency of intermolecular collisions at higher temperatures.)

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11
Q

Define Pressure Altitude:

A

The altitude that the altimeter reads if the altimeter is set to the standard sea level pressure value of 29.92. It is not corrected for local pressure variations.

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12
Q

Define Density Altitude:

What will cause an increase in density altitude?

A

Density altitude is air density given as a height above mean sea level. The more appropriate term for correlating aerodynamic performance in the nonstandard atmosphere.
Both an increase in temperature, decrease in atmospheric pressure, and, to a much lesser degree, increase in humidity will cause an increase in density altitude.

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13
Q

In the lower regions of the atmosphere temperature decreases with altitude at a fairly uniform rate up until what altitude and why?

A

Approximately 39,000’ (36,089’ = Geopotential of the Tropopause). The atmosphere is warmed by convection from Earth’s surface, this lapse or reduction in temperature is normal with increasing distance from the conductive source. There is a temperature inversion in the Stratosphere due to the ozone layer which absorbs most of the sun’s UV radiation.

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14
Q

In Bernoulli’s tube what stays constant at all stations along the length and what changes?

A

Density of the flow remains constant.Static pressure and velocity are the variable quantities.

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15
Q

Define air mass:

A

A body of air with horizontally uniform temperature, humidity, and pressure.

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16
Q

Define air pressure:

A

The force exerted by the weight of tiny particles of air (air molecules). At sea level the air pressure is 14.7 psi.

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17
Q

Define anticyclone, also known as a high pressure system:

A

A weather system with high atmospheric pressure at its center, around which air slowly circulates in a clockwise (northern hemisphere) or counterclockwise (southern hemisphere) direction - associated with calm, fine weather.

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18
Q

Define argon gas:

A

An inert gaseous element of the noble gas group (The noble gases make a group of chemical elements with similar properties: under standard conditions, they are all odorless, colorless, monatomic gases with very low chemical reactivity). Argon is the most common noble gas, making up nearly one percent of the earth’s atmosphere. Used in welding.

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19
Q

Define an atmosphere:

A

The envelope of gases surrounding the earth or another planet.

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20
Q

What are auroras and where do they occur?

A

A beautiful display of light in the sky that come from interactions between particles from the sun’s atmosphere and gases in the ionosphere.

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21
Q

Carbon dioxide:

A

A colorless, odorless gas produced by burning carbon and organic compounds and by respiration. It is naturally present in air (about 0.03 percent) and is absorbed by plants in photosynthesis.

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22
Q

Define coalescence in regards to clouds:

A

The process by which cloud droplets collide and join together to form larger droplets.

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23
Q

Define a cold front:

A

A cold front is defined as the leading edge of a cooler mass of air, replacing (at ground level) a warmer mass of air, which lies within a fairly sharp surface trough of low pressure. Temperature changes across the boundary can exceed 30 °C (54 °F). When a cold front catches up with the preceding warm front, the portion of the boundary that does so is then known as an occluded front.

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24
Q

Define condensation:

A

The change in state from a gas to a liquid

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25
Q

What are condensation nuclei?

A

Small particles in the atmosphere around which cloud droplets can form.

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26
Q

Continental polar air mass:

A

Cold arctic air masses that originate from the snow covered regions of northern Canada etc. Because of the long winter nights and strong radiational cooling found in these regions, the overlying air becomes very cold and very stable.

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27
Q

Continental tropical air mass:

A

Type of tropical air produced over subtropical arid regions; it is hot and very dry. The air has low dewpoints and warm to hot afternoon temperatures but with mild night time temperature. Skies are generally clear. This allows daytime heating during the day and radiational cooling at night.

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28
Q

Convection:

A

The transfer of energy by which a substance, such as a gas or liquid, is heated and the warmer, less dense fluid rises, then cools and becomes more dense and thus sinks.

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29
Q

Coriolis Effect:

A

The Earth’s rotation causes winds in the northern hemisphere to rotate clockwise and winds in the southern hemisphere to rotation counter clockwise

30
Q

Cyclone:

A

A system of winds rotating inward to an area of low atmospheric pressure, with a counterclockwise (northern hemisphere) or clockwise (southern hemisphere) circulation; a depression

31
Q

Dew point:

A

The atmospheric temperature (varying according to pressure and humidity) below which water droplets begin to condense and dew can form.

32
Q

Exosphere:

A

This is the outermost layer of the atmosphere. It extends from the top of the thermosphere to 6,200 miles (10,000 km) above the earth. In this layer, atoms and molecules escape into space and satellites orbit the earth.

33
Q

Greenhouse effect:

A

The phenomenon whereby the earth’s atmosphere traps solar radiation, caused by the presence in the atmosphere of gases such as carbon dioxide, water vapor, and methane.

34
Q

Isobar:

A

A line drawn on a weather map that connects points of equal atmospheric pressure.

35
Q

Isotherm:

A

A line drawn on a weather map that connects points of equal temperature.

36
Q

Jet stream:

A

A high-speed high-altitude airstream blowing from west to east. The main jet streams are located near the altitude of the tropopause, the transition between the troposphere and the stratosphere (where temperature increases with altitude).

37
Q

Land breeze:

A

The movement of air from land to sea at night, created when cooler, denser air from the land forces up warmer air over the sea.

38
Q

Latent heat:

A

Heat absorbed or radiated during a change of phase at a constant temperature and pressure, such as the melting of ice or the boiling of water.

39
Q

Lifted condensation level (LCL):

A

The height in the atmosphere at which condensation occurs.

40
Q

Maritime polar air mass:

A

Cool and moist air masses that forms over oceans due to the temperature and moisture characteristics at their source region.

41
Q

Maritime tropical air mass:

A

Originate over the warm waters of the tropics and Gulf of Mexico, where heat and moisture are transferred to the overlying air from the waters below.

42
Q

Mesosphere:

A

The layer of the atmosphere just above the stratosphere and below the thermosphere (third layer). It is the coldest part of the atmosphere and meteors burn up in this layer.

43
Q

Nitrogen:

A

A colorless, odorless unreactive gas that forms about 78 percent of the earth’s atmosphere.

44
Q

Occluded front:

A

When a cold front overtakes a warm front.

45
Q

Orographic lifting:

A

Cloud formation that occurs when warm moist air is forced to rise up the side of a mountain.

46
Q

Oxygen:

A

A colorless, odorless reactive gas and the life-supporting component of the air. Oxygen forms about 21 percent of the earth’s atmosphere, and is the most abundant element in the earth’s crust.

47
Q

Ozone:

A

Is made up of three oxygen molecules and is what protects us from the sun’s harmful UV radiation.

48
Q

Polar easterlies:

A

Prevailing winds that blow from east to west between 60-90degrees latitude in the northern and southern hemispheres,

49
Q

Prevailing westerlies:

A

Winds that blow west to east between 30 and 60 degrees in the northern and southern hemispheres.

50
Q

Radiation:

A

Is the transfer of energy through space by visible light, ultraviolet radiation, and other forms of electromagnetic waves.

51
Q

Relative humidity:

A

The amount of water vapor present in air expressed as a percentage of the amount needed for saturation at the same temperature.

52
Q

Sea breeze:

A

The movement of air from sea to land during the day when cooler air from above the water moves over the land, forcing the heated, less dense air above the land to rise.

53
Q

Stability:

A

The ability of an air mass to resist moving.

54
Q

Stationary front:

A

Boundary between two different air masses, neither of which is strong enough to replace the other.

55
Q

Stratosphere:

A

The layer of the atmosphere just above the troposphere and below the mesosphere (second layer). There is a temperature inversion (temperature increases) due to the ozone layer which absorbs most of the sun’s UV radiation.The bottom of the stratosphere is around 10 km (6.2 miles or about 33,000 feet) above the ground at middle latitudes

56
Q

Temperature Inversion:

A

Is an increase in temperature with height in the atmosphere. It occurs with the rapid cooling of land on a cold, clear, winter night when the wind is calm.

57
Q

Thermosphere:

A

The layer of the atmosphere directly above the mesosphere and directly below the exosphere (fourth layer). This is where temperatures are the highest in the atmosphere. The increasing temperature is due to the strong influence of solar activity. Within this layer, ultraviolet radiation (UV) causes ionization (northern lights).

58
Q

Trade winds:

A

Prevailing winds that blow northeast from 30 degrees north latitude to the equator and that blow southeast from 30 degrees south latitude to the equator.

59
Q

Troposphere:

A

The layer of the atmosphere that is nearest to the Earth’s surface. It is where most weather changes occur. It is the thinnest layer yet contains half of the Earth’s atmosphere.

60
Q

Warm front:

A

The boundary of an advancing mass of warm air, in particular the leading edge of the warm sector of a low-pressure system.

61
Q
Name the layers of the atmosphere:
Tr y 
S ome 
M ilk 
Th en 
E ggs
A
  1. Troposphere
  2. Stratosphere
  3. Mesosphere
  4. Thermosphere
  5. Exosphere
    Tr y
    S ome
    M ilk
    Th en
    E ggs
62
Q

Define temperature:

Standard temperature lapse rate:

A

Measure of how fast molecules are moving.

2 °C (3.5 °F) per 1,000’ change in altitude up to 38,000’

63
Q

Moist adiabatic lapse rate:

A

2.5 °C (4.5 °F)

64
Q

Solve for ISA:
11,000
FL230
FL390

A

Multiply by 2 then subtract FROM 15 °C.
11 x 2 = 22; 15 - 22 = -7 °C
23 x 2 = 46; 15 - 46 = -31 °C
FL390 N/A. Standard lapse rate is only applied up to FL380.

65
Q

The ATIS altimeter setting (QNH) is 29.79 in. Hg and the local airport elevation is 460’ MSL. What is the pressure altitude?

A

29.92 - 29.79 = 0.13 (130’)

130’ + 460’ = 590’

66
Q

Why doesn’t it continue to become colder in the Stratosphere?

A

There is a temperature inversion (temperature increases) due to the ozone layer which absorbs most of the sun’s UV radiation.

67
Q

Does an increase in humidity increase or decrease the density of the air?

A

Water vapor is a relatively light gas when compared to diatomic Oxygen and diatomic Nitrogen. Thus, when water vapor increases, the amount of Oxygen and Nitrogen decrease per unit volume and thus density decreases because mass is decreasing. Remember density is the mass of air per cubic foot and a direct measure of the quantity of matter in each cubic foot. Decreases with an increase in altitude.

68
Q

What is the danger of a slow moving warm front?

A

Imbedded thunderstorms

69
Q

What is the standard lapse rate in degrees fahrenheit?

A

3.5 degrees F / 1000’

70
Q

How would you navigate around a thunderstorm?

A

Pass it by at least 20 miles on the upwind side. You can also go over it by 1,000’ for every 10 knots of wind at the top.

71
Q

You are headed 120 magnetic on a track of 090 and there is a thunderstorm on your nose. Which way do you go?

A

South

72
Q

What are the dynamics of a Low Pressure System?

A

Unstable air

Cyclonic (counterclockwise) air flow