Exam 1 Flashcards

1
Q

The seasonal variation in the amount of energy that reaches the Earth’s surface is primarily influenced by:

A

the length of the day and the solar angle

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2
Q

When it is summer in the northern hemisphere, it is winter in the southern hemisphere.

A

True

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3
Q

During the equinoxes, the northern and southern hemispheres recieve equal illumination from the Sun.

A

True

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4
Q

At mid-latitudes, the Sun rises due east and sets due west on the summer and winter solstices.

A

False

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5
Q

On the Tropic of Cancer, the Sun is directly overhead at noon on the summer solstice.

A

True

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6
Q

Which of the following locations experiences 12 hours of daylight and 12 hours of night everyday of the year?

A

The equator

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7
Q

Which of the following locations experiences 6 months of daylight and 6 months of night?

A

The North Pole

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8
Q

On the Summer Solstice in the Northern Hemisphere, the gretest amount of solar insolation occurs at the top of the atmosphere in the Arctic.

A

True

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9
Q

On the Summer Solstice in the Northern Hemisphere, the gretest amount of solar insolation occurs at the Earth’s surface on the Tropic of Cancer (23.5° North Latitude).

A

False

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10
Q

The Earth is closest to the Sun in January (Northern Hemisphere winter).

A

True

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11
Q

Early morning heating of the air in contact with the ground is by conduction.

A

True

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12
Q

In general, air is a much better conductor of heat than the Earth’s surface.

A

False

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13
Q

The maximum daily temperature generally occurs:

A

when incoming solar energy equals outgoing surface energy

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14
Q

Daily air temperature variations are typically greater over land compared with over water.

A

True

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15
Q

When outgoing energy from the Earth’s surface excedes incoming solar energy, radiative cooling of the surface occurs.

A

True

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16
Q

As night progresses, the air in contact with the ground cools more rapidly than the air above.

A

True

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17
Q

Radiation inversions are generally most pronounced in the mid afternoon.

A

False

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18
Q

Which of the following contribute to a more pronounced night-time radiation inversion? (Check all that apply)

A

calm (windless) night
Clear skies

dry air

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19
Q

Thermal Belts develop when cold air flows down hill displacing warmer surface air to higher altitude.

A

True

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20
Q

Diurnal temperature ranges are generally smaller close to the surface and increase with altitude.

A

False

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21
Q

Diurnal temperature ranges are generally greater on clear days than on cloudy days.

A

True

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22
Q

High humidity tends to increase the diurnal temperature range.

A

False

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23
Q

The average monthly temperature is the average of the highest and lowest temperature of the month.

A

False

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24
Q

Which of the following statements is true concerning temperature changes as one moves from the equator to the pole in the winter? (Check all that apply)

A

The temperature change is greater than in the summer.

The temperature changes more over land than over the oceans.

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25
Q

The difference in the average temperature between the warmest and coldest months is greater for mid-continent than mid-ocean.

A

True

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26
Q

Locations on the western edge of a continent tend to have a greater annual temperature range than those on the eastern edge at the same latitude.

A

False

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27
Q

Potential energy can be converted to kinetic energy, but kinetic energy cannot be converted to potential energy.

A

False

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28
Q

Chemical bond energy is an example of potential energy.

A

True

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29
Q

At the atomic or molecular level, temperature is repreresented by motion. The higher the temperature the faster atoms and molecules move.

A

True

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30
Q

he Kelvin temperature scale, sets the 0 K point at absolute zero, just like the Fahrenheit scale.

A

False

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31
Q

Moist air has a higher specific heat than dry air.

A

True

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32
Q

The higher the heat capacity of a substance the more energy is required to raise its temperature.

A

True

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33
Q

Latent heat is the energy involved with a phase (gas, liquid, solid) change.

A

True

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34
Q

The evaporation of liquid water requires an input of energy, while the condensation of water vapor releases energy.

35
Q

Conduction of heat is the direct transfer of energy from one atom or molecule to another.

36
Q

Convection is the transfer of heat by the mass movement of a fluid.

37
Q

In atmspheric science, the vertical (rising or sinking) portion of a convection cell is called advection.

38
Q

As a parcel of air expands, the energy of the air molecules is reduced. This causes the parcel of air to cool.

39
Q

The range of wavelengths of visible light encompass the broadest portion of the electromagnetic spectrum.

40
Q

Radio waves have a higher frequency than visible light.

41
Q

The blackbody (or thermal) radiation emitted by an object depends only on its temperature.

42
Q

The higher the temperature of an object, the higher the peak frequency of its thermal radiation.

43
Q

The total energy emitted by an object increases by the square of its temperature.

44
Q

Molecules, such as methane, that are good absorbers at a particular wavelength of electromagnetic radiation, are also good emitters at the same wavelength

45
Q

The atmosphere near the Earth’s surface is warmed directly by incoming solar radiation.

46
Q

The Earth’s atmosphere scatters shorter wavelengths of light more effectively than longer wavelenths.

47
Q

Dark objects have a lower albedo than bright objects.

48
Q

On average, approximately half of the incoming solar radiation that hits the top of the Earth’s atmoshere makes it to the surface.

49
Q

Approximately half of the incoming solar radiation that hits the top of the Earth’s atmosphere is absorbed directly by the atmosphere and clouds.

50
Q

Compared with higher latitudes, the tropics have a surplus of energy.

51
Q

In which phase of water are the molecules moving the fastest?

A

Water vapor

52
Q

In the solid ice phase of water, the individual water molecules are bound to each other by strong covalent bonds

53
Q

In the liquid phase of water the individual water molecules are loosely bonded to each other by hydrogen bonds.

54
Q

Humidity is constant in the Earth’s atmosphere in space and time.

55
Q

Specific Humidity is defined as:

A

the mass of water vapor/mass of air

56
Q

The specific humidity of the Earth’s atmosphere is greatest near the equator and decreases steadily toward the poles.

57
Q

The process of condensation, the phase change of a gas to a liquid, requires the input of energy.

58
Q

According to Dalton’s law, the partial pressure of a gas:

A

is proportional to it’s mole fraction.

59
Q

The saturation vapor pressure:

A

is a function of temperature.

60
Q

Relative humidity is the ratio of the amount of water vapor in the air to the to the amount of water vapor required for saturation.

61
Q

If water vapor content of the air remains constant, the relative humidity will increase as temperature is increased.

62
Q

The higher the relative humitdity, the lower the dew point temperature.

63
Q

A high dew point temperature indicates a high water vapor content.

64
Q

All other things being equal, the lower the dew point temperature, the higher the expected minimum temperature.

65
Q

Relatie humidity is lowest at the oles

66
Q

Moist air is denser than dry air.

67
Q

Dew forms on objects near the ground surface when they cool below the dew point temperature.

68
Q

Dew formation is more likely on cloudy nights due to increased radiative cooling.

69
Q

White frost forms when the temperature cools below the dew point and the dew point is below 0°C.

70
Q

Condensation nuclei in the atmosphere provide the required surface for water condensation.

71
Q

Generally speaking, there are a greter number of condensation nuclei over the ocean than over land.

72
Q

The relative humidity needs to be 100% before water will condense onto condensation nuclei in the atmosphere.

73
Q

Fog forms: (Choose all that apply)

A

the saturation (dew) point

when warmer moist air is added to cooler dry air

74
Q

Radiation fog forms best on a clear night with a shallow moist layer of air near the ground.

75
Q

A light breeze will prevent the formation of radiation fog, whereas a strong breeze will promote it.

76
Q

Valley fog is produced by cold hillslope air draining down slope and ponding in the valley floor

77
Q

Advection fog forms when cool moist air moves horizontally (advects) over a warm surface.

78
Q

Air converges and rises over headlands forming fog as compared to lower elevation beaches.

79
Q

Clouds are generally classified by their altitude range and shape.

80
Q

Cirrus clouds generally form at mid-altitude - between 6 to 2 km (20,000 to 6500 ft).

81
Q

Nibostratus clouds rarely produce rain

82
Q

Stratocumulus clouds contain abundant water ice.

83
Q

Cumulonimbus clouds often extend to the tropopause.