Stratospheric Ozone Depletion (module 5) Flashcards

1
Q

Describe the structure and thermal patterns of Earth’s atmosphere, and explain where the ozone layer is located

A
  • composed of several sub-layers that differ in density, gas composition, and temperature
  • Troposphere (we live here, earth’s surface up to 20km, temp decreases with altitude due to cooling effect) - mount Everest
  • Stratosphere (50km, temp increases with altitude due to absorption of UV radiation)
  • Mesosphere (85km, temp decreases with altitude) - meteors
  • Thermosphere (690km, temp increases a lot due to absorption of high energy solar radiation) - shuttle
  • Exosphere (10000km)
  • 90% of ozone found in stratosphere (30-35 km above Earth’s surface) (comprised almost entirely of nitrogen and oxygen, high concentration of ozone)
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2
Q

Describe the role of the stratospheric ozone in the atmosphere

A
  • UV radiation absorption when intact (50% of UV-A, 90% of UV-B, and all of UV-C coming from the sun)
  • Protection of Life
  • Prevention of DNA damage
  • Climate regulation
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3
Q

Explain how the ‘hole’ in the ozone layer was first discovered, and recognize how ongoing research monitors ozone levels

A
  • Significant decline in stratospheric ozone levels over Antarctica - Dobson spectrophotometer
  • Depletion was due to man made chemicals (CFC’s)
    Monitor: satellite observations, Dobson spectrophotometer
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4
Q

Explain the three conditions needed to enable ozone destruction

A
  • UV radiation
  • Extremely low temperatures
  • A surface on which the ozone destruction process can occur (polar stratospheric clouds)
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5
Q

Describe the basic chemistry of how stratospheric ozone is created and destroyed

A
  • When high energy UV radiation from the sun breaks apart molecular oxygen
  • Oxygen atom them combines with an oxygen molecule producing a new molecule with three atoms of oxygen (ozone)
    Destroyed - ozone absorption of UV radiation
  • oxygen atom produced reacts with another ozone molecule to form two oxygen molecules
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6
Q

Identify the control variable and planetary boundary for stratospheric ozone depletion

A

Stratospheric ozone concentration (DU)
- <5% reduction from preindustrial level of 290 DU
- Only transgressed over Antarctica in southern hemisphere spring (200 DU)

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7
Q

State the main goal of the Montreal Protocol as well as why it was amended over time, and describe some of its outcomes

A
  • Plan developed to phase out CFC’s
  • Individual governments developed their own policies for reduction of CFC’s
  • amended to account for new ozone-depleting substances
  • advancements in alternative technologies
  • outcomes: reduction in ozone-depleting substances
  • protection of human health (skin cancer cases avoided)
  • environmental benefits (reducing UV radiation, minimizing damage to plants)
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8
Q

Reflect on the factors that made the Montreal Protocol an environmental policy success story

A
  • Global collaboration
  • Timely action
  • Scientific consensus
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9
Q

Explain why ozone depletion is most prevalent over Antarctica in Southern Hemisphere spring

A
  • unique atmospheric and climate conditions
  • strong stable polar vortex
  • low temperatures which lead to formation of polar stratospheric clouds
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