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Title: ozone layer depletion and its harmful effects


1
Ozone Depletion
  • What is the ozone layer?
  • How does it protect us?
  • How did it come about?

2
Evolution of the Ozone Layer
  • Early planet history
  • no ozone present
  • UV light directly hit planets surface
  • Oceans provided only refuge from UV radiation

3
Oxygen in the Atmosphere



4


UV




5
Dynamic Equilibrium
creation of ozone
breakdown of ozone
6
Anthropogenic Ozone Depletion
creation of ozone
breakdown of ozone
7
Modern Impacts to Ozone
  • Chlorofluorocarbons (CFCs)
  • What are they?
  • How do they impact the ozone layer?

8
Development of CFCs
  • 1928 DuPont scientists develop CFCs
  • ideal compounds for
  • refrigerants and propellants
  • WHY??

9
CFCs as Refrigerants
  • vs. CFCs
  • Non-flammable
  • Non-toxic
  • Trap heat (good insulators!)
  • Inexpensive
  • Light
  • Extremely stable, inert
  • Traditional Refrigerants
  • (ammonia, sulfur dioxide, methyl chloride)
  • Highly volatile
  • Caustic and toxic
  • Remove heat through vaporization of
    liquefied gas (only adequate as
    refrigerants)
  • Expensive
  • Heavy (transport, storage)

10
CFCs as Propellants
  • Light weight
  • Extremely stable or inert

What are the consequences of these two physical
characteristics?
  • CFCs likely to migrate upwards
  • Too light to precipitate out with rainfall
  • 5-15 years to migrate to stratosphere

11
Marketing of CFCs
  • 1958 DuPont releases CFCs on the market
    commercially
  • 1971 James Lovelock speculates that CFCs
    put into the atmosphere may still be
    present
  • 1973 Mario Molina and F. Sherry Roland
    start to investigate

12
Original Research
  • 1974 Rowland and Molina



Cl- free radical
13
Cl- Free Radicals




14
In the news
  • 1974 Molina and Rowland publish their
  • hypothesis in Nature.
  • New York Times runs front page
  • DuPont responds with study showing that
    CFCs in troposphere are benign

15
High Risk and Political Savvy
  • 1975 200 increase in CFC use from 1968, only
    eight years
  • 1979 The FDA, EPA ban non-essential uses of
    CFCs !
  • First time substance EVER banned without
    direct proof of harm
  • 1982 20 other countries join US in ban of CFCs

16
Scientific Controversies
  • 1982 British science teams in Antarctica
    observe 20 decline in O3 layer
  • US scientists relying on TOMS (Total Ozone
    Mapping Spectrometer) measurements from
    space claim to observe nothing

17
Scientific Evidence
  • 1983 British scientists observe 30
    reduction in ozone layer.
  • US scientists claims no reduction.
  • 1985 British observe 50 reduction.
  • US claims no reduction.
  • US re-tests and confirms.
  • WHY THE SCIENTIFIC SNAFUS??

18
Total ozone
Total ozone measured above Antarctica,
in Dobson Units. From Horel and Geisler, 1996
19
TOMS Data (corrected)
20
October Average for Total Ozone over Antarctica,
1955-1995 Based on British measurements from
weather balloons
21
Understanding the Science
  • 1986 DuPont scientists continue to argue that
    tropospheric ozone (smog) will migrate up and
    fill the ozone hole in the stratosphere
  • Why doesnt this theory fly?

22
Location of Stratosphere
23
Montreal Protocol Landmark
  • 1987 2 yrs of intensive research reveal that
    ozone hole is anthropogenic
  • 1988 UN hold meeting in Montreal
  • 45 Nations sign to reduce CFC use by 50 by
    year 2000.
  • Developing countries efforts would be
    subsidized

24
Two steps forward
  • 1990- Follow up meetings result in
  • 1992 Industrialized nations total ban by 2000
  • Developing nations ban by 2010, with
    assistance from developed nations
  • US agrees to complete phaseout by 1996 DuPont
    to halt production by 1997
  • 1995 Rowland and Molina receive Nobel Prize

25
One step back
  • 1995 Congress challenges ozone science
  • Junk science gains credibility
  • despite scientific consensus of
    anthropogenic causes of O3 depletion
  • 1996 Ban begins but black market for CFCs appear
  • WHY?
  • CFC substitutes (HFC) break down faster, but
    still pose problems for ozone depletion

26
Modern Impacts to Ozone (2)
  • Methyl Bromide
  • What is it?
  • Challenges to Montreal Protocol

27
Methyl Bromide
28
Uses of Methyl Bromide
  • 60 million lbs /yr in US
  • Agricultural (75)
  • Strawberries
  • Stored products (11)
  • Flame retardants (6)
  • Pest management (6)
  • Termite removal
  • Chemical production (2)

29
Schedule for Elimination
  • 1991 Designated Class I ozone depleter in
    Montreal Protocol
  • 1997 Agreed to following schedule
  • Developed Countrieselimination by 2005
  • Developing Countrieselimination by 2015
  • Requests for Critical Use Exemptions

30
US Strawberry Industry
  • US supplies 80 of plants from nurseries or
    strawberries to world market
  • Average consumption
  • 4 lb/person/yr

31
Benefits of Methyl Bromide
  • Worker safety
  • Non-toxic
  • Reduces need for toxic pesticides
  • Economical
  • Easy-to-Use
  • Effective

32
Alternatives
  • Fumigants applied through drip irrigation
  • Harnessing good microbes
  • Composting for weed suppression
  • Soil solarization
  • Crop rotation

33
Effectiveness
  • Other fumigants do not work
  • Worker health issue
  • Lower yields
  • Loss of nurseries
  • Even organic farms get plant stocks from
    nurseries that rely on methyl bromide

34
CFCs vs MEBr
  • Why did one industry eventually support ban
    while another is struggling and begging for
    exemptions?

Methyl Bromide CFCs -no viable alternatives
-DuPont developed HFCs
35
Another potential threat?
Hydrogen Fuel Cells
36
Production of Hydrogen
  • Anticipate that 10 of all hydrogen manufactured
    will leak into the atmosphere during production,
    storage and transport.
  • Current loss is higher
  • Estimate 60 million tons / year
  • Roughly doubles current input (all sources)

37
Hydrogen chemistry
  • Hydrogen is lightrises rapidly to stratosphere
  • Reacts with oxygen to form water
  • A wetter atmosphere would cool the lower
    stratosphere, especially around Poles
  • Increase in water vapor is catalyst for ozone
    depletion by freeing Cl free radicals

38
Spatial and Temporal Patterns
  • Poles have greater ozone loss than other regions
  • Colder
  • More vapor formation
  • Also polar vortex
  • Particularly severe in polar spring (October)
  • Increased hydrogen would enhance this phenomenon

39
Ozone Layer Impacts
  • 7-8 depletion around Poles anticipated
  • Depends upon if and how quickly hydrogen economy
    introduced
  • If gt50 years, may not be critical issue
  • Possible work to lessen H leakage

40
Current Status of Ozone Hole
  • Extent of ozone depletion
  • 1981 900,000 sq mi
  • 200117,100,000 sq mi

41
Location of Ozone Losses
  • Ozone loss extends beyond Antarctica and Arctic
    Polar regions
  • Ozone loss over US currently 5 below normal
    rates

42
Current Rate of Ozone Depletion
  • Decrease in rate of ozone depletion (since 1997)
  • Slowing of buildup of harmful Cl- from CFCs
  • Ozone hole is still growing, but
  • Models anticipate restoration of normal
    balance of ozone in stratosphere by 2050

43
Impacts of Ozone Depletion
  • Human Health
  • Skin cancer
  • Melanoma
  • Cataracts
  • Immune system function
  • Increased incidence, severity and duration of
    infectious diseases
  • Reduced efficacy of vaccinations
  • Ecological Health
  • Pathogen locally up down
  • Biodiversity locally up down
  • Aquatic organisms adversely impacted
  • Decreased biomass productivity
  • Polar systems especially vulnerable

44
Impacts of Ozone Depletion
  • Economic
  • Plastics
  • designed with stabilizers to withstand UV
    radiation of certain intensity
  • replacement of key medical equipment and
    supplies, decreased lifespan of plastics
  • Manufacturing practices
  • Agriculture
  • Consumer costs and burdens

45
Breakdown of Sources
46
Success Story
  • What characteristics define ozone depletion
  • an environmental success story ?
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