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What are the wavelengths of harmful UV radiation?
UVB: 280-320 nm
UVC: <280 nm
Why is ozone particularly generated in the tropics?
More sunlight
More lightning
Give the 4 stages of the Chapman cycle
Photolysis (1)
Recombination
Photolysis (2)
Bimolecular reaction
Give the equn of photolysis (1)
O₂ + hv→ O + O
hv: <240 nm
Give the equn of recombination
O + O₂ + M→ O₃ + M
Give the equn of photolysis (2)
O₃ + hv→ O₂ + O
hv: <310 nm
Give the equn of the biomolecular reaction
O₃ + O→ 2O₂
Why is recombination non-arrhenius?
pressure dependant
Why was there a discrepancy between calculations based off the chapman mechanism and observations?
Calculations overestimated ozone conc
sinks too low, in reality: catalytic cycle
Why are catalytic cycles important in ozone depletion?
trace amounts can destroy large amounts of ozone as they are not used up in a reaction so can go on to react many times before they are destroyed
Give a more accurate version of the last step of the chapman cycle
X + O₂→ XO+ O₂
XO+ O→ X + O₂
where X = H, OH, NO, Cl, Br
What is the range of wavelengths that CFCs absorb to release Cl.?
180-230 nm
Where does photolysis of CFCs take place?
suitable wavelengths only found in stratosphere
What is the ozone column?
The total integrated amount of ozone from the top of the atmosphere to the bottom over 1cm3
in Dobson units- 10^5 ozone molecules per cm3
What was early evidence of ozone depletion?
upward facing observations of ozone column in antarctica showed decline
What were the inital expectations of ozone depletion?
uniform, gradual depletion throughout stratosphere
What was surprising about ozone depletion?
strong, localised depletion
Why was alarm not initially raised?
potentially in line with interannual variation
How did ozone depletion vary with altitude?
Little to no ozone between 14-20 km where there had previously been a peak
other regions unaffected
Why did ozone depletion take place in the antarctic?
colder in winter than the arctic (-80 deg), leads to polar stratospheric cloud formation
polar vortex forms during the dark winter months which isolates the air from the rest of the atm
What are polar stratospheric clouds?
rare due to low mol fraction of water in stratosphere
only form in v low temperatures where water and nitric acid condense on sulf. acid containing particles
correspond to the altitude at which ozone depletion takes place
What are the breakdown products of CFCs?
HCl
ClONO2
which descends into polar vortex and serve as reservoirs
Describe ozone depletion in PSCs (words)
HCl + CLoNO2 adsorbed onto PSC surfaces react to form Cl2
Cl2 released into atm due to higher vapour pressure and builds up over polar winter
Cl2 photolyses in spring/summer to give Cl radicals
Cl radicals take part in catalytic cycles to deplete ozone
Describe ozone depletion in PSCs (equns)
HCl + ClONO₂→ HNO₃ + Cl₂
Cl₂ + hv→ Cl + Cl
Cl + O₃→ ClO + O₂
ClO + O→ Cl + O₂ OR ClO + ClO + M ⇌ ClOOCl + M (lower strt)
ClOOCl + hv→ Cl + Cl + O₂ (lower strt: cold temp, high presh)
Why is ozone depletion important?
Changes optical depth of column in UV
More UV reaches surface: skin cancer, eye cataracts, damage to plants and phytoplankton, photo oxidation of building materials
What about an arctic ozone hole?
arctic stratosphere becoming colder and more humid
suitable conditions for PSC
could lead to arctic ozone hole
What were the steps of solving the problem?
Vienna convention (1985) set out need to protect ozone layer
Montreal protocol (1987-1989): technology fund allows transition away from CFCs. Initial obligation to reduce production + consumption of CFCs by 50% by 1999. Amendment in 1990+1992 to bring forward pace of phase-out
What were the unintended consequences of CFC replacements?
excellent greenhouse gases- absorbed in a previously untouched region of IR
changed radiation budget- large greenhouse effect
What was the purpose of the Kigali amendment?
legally binding reduction of HFCs (replacement CFCs) by 80% by 2047