6.1 Introduction to the Atmosphere Flashcards

1
Q

Atmosphere definition

A

a dynamic system (with inputs, outputs, flows and storages) that has undergone changes throughout geological time.

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2
Q

Atmosphere Inputs

A
  • Water (evaporation and transpiration)
  • CO2, SO4 and NO2 from combustion
  • Volcanic ash
  • Solar radiation
  • oxygen through photosynthesis
  • aerosols
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3
Q

Atmosphere outputs

A
  • precipitation
  • solar radiation
  • oxygen for respiration
  • CO2 for photosynthesis
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4
Q

Amount nitrogen

A

78%
- dilutes oxygen
- prevents rapid burning at the earth’s surface
- living things need it to make proteins

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5
Q

Amount oxygen

A

21%
- passive importance to weather and climate
- produced by photosynthesis
- reduced by deforestation
- needed for animal life

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6
Q

Amount argon

A

0.9% - Used in light bulbs.

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7
Q

Amount carbon dioxide

A

0.04%
- absorbs long wave radiation from earth and therefore contributes to natural greenhouse effect
- increases due to human activity is a major cause of global warming
- used by plants for photosynthesis
- increased by burning fossil fuels and deforestation

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8
Q

Amount water vapour

A

0.2 - 4.0%
- source of cloud formation and percipitation
- reflects/absorbs incoming radiation
- keeps global temp. constant
- provides majority of natural greenhouse effect
- essential for life

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9
Q

Atmosphere levels

A
  1. troposphere
  2. stratosphere
  3. mesosphere
  4. thermosphere
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10
Q

Troposphere

A
  • fall in temp with height as atmosphere thins
  • Most of the atmospheric mass is found.
  • Most of our weather occurs here.
  • Humans and other organisms have most interaction e.g. through exchange of gases or through introduction of pollutants.
  • Greenhouse gases (GHG) help to regulate the temperature of the earth.
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11
Q

Mesosphere

A
  • Temperature declines with height
  • Coldest part of the atmosphere.
  • density prevents absorption of energy
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12
Q

Stratosphere

A
  • Temperature is constant at about -60°C in the lower part of the stratosphere, which is shielded by the ozone layer but then increases with altitude.
  • The air is dry.
  • stable
  • thin
  • increase in temp with height is due to absorption of solar radiation
  • Ozone layer at the top of the stratosphere. Stratospheric ozone absorbs ultra violet radiation from the sun
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13
Q

Thermosphere

A
  • Temperatures climb sharply in the lower thermosphere (below 200 to 300 km altitude), then level off and hold fairly steady with increasing altitude above that height.
  • virtual vacuum
  • rise in absorbed energy due to energised short wave radiation
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14
Q

Albedo definition

A

a measure of the reflectivity of a surface.

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15
Q

Albedo effect

A

when applied to the Earth is a measure of how much of the Sun’s energy is reflected back into space

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16
Q

Albedo effect on clouds

A

More water vapour in the atmosphere means more cloud formation. More clouds lead to increased albedo of the earth.
- Different parts of the Earth have different albedos.

17
Q

About how much of incoming solar radition is reflected back into space?

A

about 30% (shortwave radiation)

17
Q

What is the greenhouse effect

A

a natural and necessary process in which greenhouse gases allow short wave radiation (visible light and UV) to pass through the atmosphere but trap a percentage of the outgoing long wave radiation (infrared radiation).
increases global temps. by about 30C → allowing life on earth

18
Q

Discuss the role of the albedo effect from clouds in regulating global average temperature.

A
  • The proportion of incident radiation reflected by a substance is called albedo.
  • Low thick clouds, like stratus, have high albedos around 90%.
  • High thin clouds, such as cirrus, have lower albedos, approximately 10%.
  • Cloud albedo remains consistent across different wavelengths of visible light, indicating their white appearance under white light.
  • During sunrise and sunset, clouds reflect the red, orange, or yellow light without modification, showing wavelength independence.
  • The albedo of clouds for infrared radiation is likely similar to that for visible light.
  • Clouds have two reflective surfaces: the top and bottom, which both play roles in radiation reflection.
  • A higher albedo means more solar radiation is reflected back into space, potentially cooling the planet.
  • Conversely, a lower albedo results in more solar radiation being absorbed, which can increase Earth’s temperatures.
19
Q

Outline the role of the greenhouse effect in regulating temperature on Earth

A
  • An atmospheric heating phenomenon where the Earth experiences a rise in temperature.
  • Certain gases such as water vapor, carbon dioxide, nitrous oxide, and methane allow incoming sunlight to pass through but trap heat radiated from the Earth’s surface.
  • If these gases did not trap heat, the Earth’s average temperature would be about 33 degrees centigrade colder.
  • These gases are termed greenhouse gases due to their role in warming the planet, creating the greenhouse effect.
  • Incoming solar thermal radiation, or heat, is partially reflected by the ozone layer, which blocks the most harmful solar radiation.
    The heat that reaches the - Earth is then re-radiated upwards but is mostly trapped by greenhouse gases, causing it to remain within the Earth’s atmosphere.
20
Q

how do humans impact the atmospheric composition?

A

through altering inputs and outputs of the system

21
Q

what is the enhanced greenhouse effect?

A

the anthropocentric/human induced global warming as a result of increased use of greenhouse gases

22
Q

main human activities releasing greenhouse gases/enhancing greenhouse effect

A
  • burning fossil fuels (coal, oil gas) → releasing co2
  • deforistation → takes away co2 store → releases more co2 into atmosphere
  • fertiliser in agricultural systems → higher nitrous oxide concentration when fertilisers break down
23
Q

GHG in the atmosphere

A

water vapour, co2, methane, nitrous oxide, CFCs and HCFC

24
Q

Atmosphere processes

A
  • respiration
  • photosynthesis
  • percipitation
  • dry deposition