Ozone Depletion Flashcards
Module 2: The Physical Environment
Explain stratospheric ozone and how it is in equilibrium.
In O3 form in the stratosphere around 12-24km above Earth’s surface. O3 is in dynamic equilibrium with of chemical reactions caused by absorption of ultraviolet light
Explain the importance of stratospheric ozone?
It prevents most of the high-energy ultraviolet solar radiation from reaching Earth’s surface.
Categorise UV light by its wavelength, with its characteristics.
UV A: 320-400nm and not absorbed by ozone or diatomic oxygen (O2).
UV B: 280-320nm and almost fully absorbed by ozone.
UV C: <280nm. Completely absorbed by ozone and diatomic oxygen (O2).
Explain the formation of ozone in steps:
1, UV light splits a molecule of O2
2. Monatomic (O) reacts with Diatomic (O2) to form O3 (ozone).
Explain the destruction of ozone in steps:
- UV light splits an ozone molecule
- O3 will be split into one O2 molecule and an O atom.
How does UVB light effect living organisms.
If UVB is not absorbed in the atmosphere then it will reach the Earth’s surface and my be absorbed by living cells. The energy of UVB is absorbed and some is converted to chemical energy as its breaks up biological molecules causing skin damage, skin cancer, DNA damage, cataracts (cloudy eye), leaf tissue damage and reduced photosynthesis, and damage to marine organisms.
What properties did made CFCs ideal to aircon units, aerosols, and refrigerants
- Boiling points close enough to ambient temperatures that the gases can be liquefied with easily achievable pressures. So aerosol cans did not need to be very strong and compressors in fridges and AC units did not have to be powerful.
- Ability to dissolve grease and oils but not damage electrical components.
- CFCs are not flammable.
- Most are non-toxic.
What is the Rowland-Molina hypothesis:
In 1974, two American research scientists suggested that the chemical properties of CFCs could lead to ozone depletion. Their theory was based on the chemical behaviour of CFCs.
1. Persistence of CFCs
2. Dissociation by UV and the release of Chlorine.
3. Reaction of Chlorine and Oxygen
How is ozone measured?
Dobson Units (DU), which estimates the total thickness of all the ozone in the atmosphere as if it existed as a layer of pure ozone at sea level.
100DU is equivalent to 1mm thick ozone layer, normal ozone levels are around 300DU.
What level of DU is considered an Ozone hole
Around 220DU
Explain ground-based data collection of ozone
The first evidence of ozone depletion was collected by the British Antarctic Survey at Halley Station in Antarctica. The detection of higher levels of UV at the ground level was evidence of ozone loss in the atmosphere.
Explain Satellite surveys for ozone data
Satellites orbit Earths at greater altitudes than the stratosphere so UV passing downwards through the stratosphere cannot be measured. However reading of UV light reflected by the Earth were higher than expected, suggesting ozone levels were reduced.
Explain air samples from the stratosphere
Ground-based and satellite surveys showed high UV levels as evidence of ozone depletion but could not confirm the cause, or detect any changes in the chemistry of the stratosphere. Air samples collected by helium balloons and high-flying research aircraft confirmed the chemicals that were causing depletion, especially chlorine and chlorine monoxide.
Explain how ozone levels vary
Ozone concentration varies in different areas, at different times, and at different altitudes
Where is ozone depletion most severe?
At altitudes of 12-24km where UV light splits ozone molecules, releasing monatomic oxygen that can react with chlorine, preventing to reformation of ozone.
Over Antarctica where levels have sometimes dropped below 100DU.
During September to December in Antarctica.