Atmosphere: The Global Heat Budget Flashcards

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1
Q

most significant layers of atmosphere (2)

A
  • troposphere
  • stratosphere
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2
Q

troposphere

A
  • contains most atmospheric moisture
  • most air, water vapour and dust
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3
Q

stratosphere

A
  • contains ozone gas which filters out the most harmful UV radiation
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4
Q

total insolation reflected

A

30%

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5
Q

total insolation absorbed

A

70%

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6
Q

total insolation absorbed by the earth

A

51%

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7
Q

insolation can be reflected/absorbed by… (3)

A
  • clouds
  • atmospheric particles
  • earth’s surface
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8
Q

different rates of reflection can be explained by… (3)

A
  • different cloud cover
  • whiteness of snow/ice in polar areas
  • deserts
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9
Q

different rates of absorption can be explained by… (2)

A
  • smog over cities
  • dark surfaces of ocean and rainforest in tropical areas
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10
Q

how does earth’s curvature affect the angle of insolation?

A
  • at the equator, insolation hits the earth at a right angle and is more intense
  • at the poles, insolation hits the earth at an oblique angle and is weaker
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11
Q

how does earth’s curvature affect the area of insolation?

A
  • at the equator, insolation is concentrated on a smaller area
  • at the poles, insolation is spread out over a larger area
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12
Q

how does earth’s curvature affect the amount of atmosphere that insolation has to travel through?

A
  • at the poles, insolation has to travel through more atmosphere, so more energy is lost
  • at the equator, insolation has to travel through less atmosphere, so less energy is lost
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13
Q

how does the Albedo effect affect the amount of insolation received by the poles/equator?

A
  • at the poles, the whiteness of ice and snow reflect the solar radiation
  • at the equator, the dark colour of the oceans and rainforest absorb solar radiation
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14
Q

how does seasonal variation affect the amount of insolation received by high/low latitudes?

A
  • at lower latitudes in the tropics, the sun is high in the sky all year, so high amounts of insolation are received all year
  • at higher latitudes, there are distinct hot and cold seasons, so some areas receive less insolation for several months a year
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