Stratospheric Ozone Depletion (module 5) Flashcards
Describe the structure and thermal patterns of Earth’s atmosphere, and explain where the ozone layer is located
- 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)
Describe the role of the stratospheric ozone in the atmosphere
- 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
Explain how the ‘hole’ in the ozone layer was first discovered, and recognize how ongoing research monitors ozone levels
- Significant decline in stratospheric ozone levels over Antarctica - Dobson spectrophotometer
- Depletion was due to man made chemicals (CFC’s)
Monitor: satellite observations, Dobson spectrophotometer
Explain the three conditions needed to enable ozone destruction
- UV radiation
- Extremely low temperatures
- A surface on which the ozone destruction process can occur (polar stratospheric clouds)
Describe the basic chemistry of how stratospheric ozone is created and destroyed
- 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
Identify the control variable and planetary boundary for stratospheric ozone depletion
Stratospheric ozone concentration (DU)
- <5% reduction from preindustrial level of 290 DU
- Only transgressed over Antarctica in southern hemisphere spring (200 DU)
State the main goal of the Montreal Protocol as well as why it was amended over time, and describe some of its outcomes
- 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)
Reflect on the factors that made the Montreal Protocol an environmental policy success story
- Global collaboration
- Timely action
- Scientific consensus
Explain why ozone depletion is most prevalent over Antarctica in Southern Hemisphere spring
- unique atmospheric and climate conditions
- strong stable polar vortex
- low temperatures which lead to formation of polar stratospheric clouds