Deck 5: Radiation and the Heat Balance of Planet Earth
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Deck 5: Radiation and the Heat Balance of Planet Earth
1
The amount of solar radiation reflected off a surface on Earth is called:
A) albedo
B) insolation
C) diffusivity
D) emissivity
E) color quotient
A) albedo
B) insolation
C) diffusivity
D) emissivity
E) color quotient
A
2
Greenhouse gases are most efficient at absorbing ________ wavelengths of energy.
A) visible
B) ultraviolet
C) infrared
D) microwave
E) shorter
A) visible
B) ultraviolet
C) infrared
D) microwave
E) shorter
C
3
The planetary albedo of the Earth is about _____ percent.
A) 10
B) 17
C) 33
D) 45
E) 50
A) 10
B) 17
C) 33
D) 45
E) 50
C
4
The greenhouse gas most effective at absorbing heat is:
A) carbon dioxide
B) methane
C) water vapor
D) CFCs
A) carbon dioxide
B) methane
C) water vapor
D) CFCs
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5
Much of the Earth's heat escapes between the wavelengths of 8.5 and 13 micrometers, which is also called:
A) the gap
B) the atmospheric window
C) the atmosphere's door
D) ozone hole
A) the gap
B) the atmospheric window
C) the atmosphere's door
D) ozone hole
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6
The solar constant is:
A) the total energy emitted by the sun
B) the total solar energy absorbed by the Earth's surface
C) the total solar energy reaching the top of the atmosphere
D) none of these
A) the total energy emitted by the sun
B) the total solar energy absorbed by the Earth's surface
C) the total solar energy reaching the top of the atmosphere
D) none of these
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7
The Earth's re-radiation of heat back towards space is mostly in the ____ wavelengths.
A) visible
B) ultraviolet
C) infrared
D) microwave
E) radio
A) visible
B) ultraviolet
C) infrared
D) microwave
E) radio
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8
If it was not for the greenhouse effect, the Earth's average temperature would be about ____.
A) -20°F
B) 0°F
C) 32°F
D) 50°F
E) 65°F
A) -20°F
B) 0°F
C) 32°F
D) 50°F
E) 65°F
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9
To be in perfect equilibrium, the Earth's net radiation must be:
A) -10% of the solar constant
B) 0% of the solar constant
C) 10% of the solar constant
D) 25% of the solar constant
A) -10% of the solar constant
B) 0% of the solar constant
C) 10% of the solar constant
D) 25% of the solar constant
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10
Global net radiation is:
A) positive in the tropics, negative in the polar regions
B) positive in the polar regions, negative in the tropics
C) positive at all latitudes
D) zero at all latitudes
A) positive in the tropics, negative in the polar regions
B) positive in the polar regions, negative in the tropics
C) positive at all latitudes
D) zero at all latitudes
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11
When heat is transferred between warm and cooler layers of soil in contact with one another, it is termed:
A) convection
B) conduction
C) radiation
D) sensible heat
A) convection
B) conduction
C) radiation
D) sensible heat
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12
An increase in Earth's albedo would lead to:
A) an increase in global temperature
B) a decrease in global temperature
C) no change in global temperature
A) an increase in global temperature
B) a decrease in global temperature
C) no change in global temperature
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13
More incoming energy is used at the Earth's surface for ______ at an ocean surface.
A) sensible heat
B) latent heat
C) heating the subsurface
D) cooling the subsurface
A) sensible heat
B) latent heat
C) heating the subsurface
D) cooling the subsurface
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14
Heat is transferred from lower latitudes toward higher latitudes mainly by:
A) atmospheric winds
B) oceanic currents
C) both (a) and (b)
D) neither (a) and (b)
A) atmospheric winds
B) oceanic currents
C) both (a) and (b)
D) neither (a) and (b)
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15
In colder climates during winter, heat is conducted:
A) from the surface downward
B) from the air towards the ground
C) from the subsurface towards the surface
D) neither upward nor downward below the surface
A) from the surface downward
B) from the air towards the ground
C) from the subsurface towards the surface
D) neither upward nor downward below the surface
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