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SIT ANYWHERE YOU LIKE TODAY!
TODAY: TOPIC #14
OZONE DEPLETION
Tuesday Nov 10th
• GC SAVVY COMSUMER PROJECT:
Deliverable #1 is due before MIDNIGHT TONIGHT!
(go to D2L to find the link to submit it)
• RQ-8 is DUE Thu Nov 12 (30 min before class)
• Some class time will be provided on Thursday for
your groups to strategize on your GROUP’s GC topic
presentation.
IMPORTANT GUIDELINES on the
GC SAVVY COMSUMER PROJECT:
Purpose of the assignment is to link the GLOBAL
CHANGE TOPICS OF THIS CLASS with your everyday life
– so your consumer product research / selection criteria
MUST have a direct link to at least ONE of our CLASS
TOPICS! e.g.:
-Ecological Footprint / Carbon Footprint (food choices/
vegetarian diet, transport vs. local food)
- Electromagnetic Spectrum & harmful UV radiation, ozone
depletion issues
- The balance between auto crashworthiness (Laws of
Motion) and fuel economy (GH Gas Emissions)
- Energy Efficiency ( solar, electronics w/ energy Star ratings)
- Deforestation / Sustainability (paper products,
recycling, etc.)
Topic # 14
OZONE DEPLETION
IN THE
STRATOSPHERE
see pp 75-79 in Class Notes
“[ The Ozone Treaty is ] the
first truly global treaty that
offers protection to every
single human being.”
~ Mostofa K. Tolba,
Director of the UN Environment Programme
SEPTEMBER 16th
http://www.timeanddate.com/holidays/un/international-ozone-layer-preservation-day
Generally, the Self Tests have been very useful for me in
this class. I like how they summarize the major points of
each topic and the help they provide on the RQ’s. They also
are a good reference to use while studying for tests. 
To me, the self-tests are extremely useful. I love being able to
read the question, my choices for an answer, and then
automatically being able to learn whether or not I was correct.
Not only do I like being able to see how I did answering the
question, but there is an explanation as to why the answer is
correct or incorrect, which is very very useful for studying! I’m
very grateful!
I think the self tests are very useful because they prepare you
well for the Readiness quiz after you have read the material. I
almost get a 5 every time because of these self tests. I am
thankful for the help.
SELF TEST
BONUS POINT !!
The real answer:
The ozone hole is:
-- a depletion of
ozone in the lower
stratosphere
-- that has occurred
with increasing
severity each
spring (since
measurements begin in
1970s)
NOTE: the “Key Concepts”
are all provided on p 79
OZONE STORY = A very interesting
illustration of the scientific process!
The THEORY that the ozone layer in the
stratosphere might be damaged by human
intervention PRECEDED the actual
OBSERVATION of the ozone hole.
Yet, when the hole WAS observed (via
satellite) it was almost “missed” because it
wasn’t expected . . .
Key Concept
But let’s begin with the stratospheric
ozone layer itself . . . . . .
WHERE IS THE OZONE LAYER?
Stratosphere
Ozone Concentration (ppm)
SGC
Fig. 3-11

OZONE: Sources
Ozone is produced naturally in
photochemical reactions in the
stratospheric ozone layer --“good
ozone” -- is decreasing!
However, ozone has increased in
troposphere due to photochemical
smog reactions -- “bad ozone” review
Here’s a
different version
of the figure 
Shows 2 peaks,
a major peak in
O3 density in the
stratosphere, a
smaller
secondary peak
in the lower
troposphere
Ozone Density
(1017 molecules / m3) p 76

22 km altitude peak 
Bulk of ozone produced
at ~ 25 km & drifts downward
Another lesser peak at ground level
First we’ll focus
on the “GOOD”
ozone located
in the
STRATOSPHERE
(the ozone that is
being depleted
leading to an
ozone “hole”)
THE OZONE LAYER IN THE
STRATOSPHERE --
WHY IT'S THERE
Due to: the natural
“Chapman Mechanism”
(a series of photochemical reactions)
 ozone is continuously produced
and destroyed
 through PHOTOCHEMICAL
REACTIONS in the stratosphere
 involves oxygen (O2), molecular
oxygen (O), photons of UV
radiation, and OZONE (O3).
THE CHAPMAN MECHANISM
(first proposed in 1930s)
Key Concept
O
O
O O
O
O
O
O O
O
O
O O
O
+
+
The Chapman
Mechanism
p 75
O O
O
O O
O
O O
O
O
O
O O
O

The Chapman Mechanism
(another view)
[Go to movie clip]
Ozone being
formed
naturally
Ozone being
destroyed
naturally
Ozone being
destroyed
naturally
Ozone being
formed
naturally
p 75
In theory:
a balance of ozone is
established over time
> prevents much of the
harmful UV radiation from
reaching the earth's surface.
Leads to an “Equilibrium” or
“Steady State”
Key Concept
STEADY STATE =
a condition in which
the STATE of a
system component
(e.g. reservoir)
is CONSTANT
over time.

Steady state can be
achieved
in a reservoir:
a) if there are no inflows
or outflows, or
b) if the rate of inflow =
the rate of outflow.
Any imbalance in these
rates leads to a change
in the level of the
reservoir.

FLOW DIAGRAM
OF A STEADY STATE
Reservoir
of
STRATOSPHERIC
OZONE
Inflow
Ozone being
formed via
natural Chapman
mechanism
Outflow
Ozone being
destroyed via
natural Chapman
mechanism
Stratospheric ozone under steady
state natural conditions
Ozone reservoir
After an initial
period of
adjustment
a steady state is
reached  as a
horizontal line 
Review:
Why stratospheric
ozone is “Good”:
p 75
Ozone has the property
of being a very strong
absorber of ultraviolet
radiation  nearly total
absorption of
wavelengths less than
0.3 m
Black areas = radiation absorbed
 remember
this figure?
Circle the CORRECT completion to
this sentence:
The global change issue usually
referred to as Stratospheric Ozone
Depletion is related to the part of the
absorption curve that is labeled ____.
X or Y
1. . . . because X represents UV radiation being absorbed --
hence if ozone is depleted, MORE ultraviolet radiation will
reach the Earth’s surface.
2. . . . because X represents terrestrial longwave radiation
being absorbed -- and hence serves as a catalyst in the
Chapman mechanism.
3. . . .because X represents easy transmission of
wavelengths of terrestrial longwave radiation out to space
which then disappear through the “atmospheric window”
also known as the ozone hole.
Ok, X is right, but Why?
Ozone Density graph
Temperature graph
Now roughly sketch
the temperature line
from this graph onto
the ozone graph
First sketch in
tropopause &
stratopause
p. 38 in Class Notes:
p 76
TEMPERATURE
[ increases / decreases ]
with increasing altitude
in the stratosphere
WHY???
p 76
1. It is the closest layer to the sun, hence it is
closest to the solar “heat source.”
2. It receives large amounts of UV radiation
from the sun PLUS it has a high
concentration of ozone to absorb this UV.
3. It is the layer which contains most of the GH
gases that absorb IR radiation emitted by the
Earth’s surface.
Why is there an increase in temperature with
altitude in the STRATOSPHERE?
What about the “BAD” ozone
located in the troposphere?

Ozone has increased in
troposphere due to
photochemical smog
reactions  “bad ozone”
HEALTH AND ENVIRONMENTAL EFFECTS OF
GROUND-LEVEL OZONE
Why are We Concerned
about Ground-Level Ozone?
 Ozone is the prime ingredient
of smog in our cities and
other areas of the country.
http://www.epa.gov/ttn/oarpg/naaqsfin/o3health.html

 When inhaled, even at very low
levels, ozone can:
• cause acute respiratory problems
• aggravate asthma
• cause significant temporary decreases
in lung capacity
• cause inflammation of lung tissue
• lead to hospital admissions &
emergency room visits
• impair the body's immune system
defenses
http://www.epa.gov/ttn/oarpg/naaqsfin/o3health.html


“BAD” OZONE
Ground-level ozone is a form of pollution
created when:
nitrogen oxides in auto emissions
+ hydrocarbons from plant matter
+ solvents and gasoline fumes
. . . . mix and bake in stagnant heat and sunlight!
http://www.airinfonow.org/html/ozoneMC.html
Tucson data
ANOTHER LINK TO
EVERYDAY LIFE:
SUN SAFETY!
UVA
UVC
UVB Turn to p 75
%
UV
C-B-A
OZONE / Oxygen
Absorption Curve
p 75
UV-C
wavelengths are
the most
harmful
Wavelength
Range Name Biological Effect
.32 to .4 m
(320-400 nm)
UVA
(SPF doesn’t rate
UVA protection!)
once thought to be relatively
harmless, BUT causes
wrinkles, premature aging
and associated sun-related
skin damage; new research
indicates possible skin
cancer link
.29 to .32
m
(290-320 nm)
UVB
(see SPF for
protection)
harmful, causes sunburn,
skin cancer, and other
disorders
.20 to .29
m
(200 - 290 nm)
UVC
(almost
completely
absorbed by O3)
extremely harmful, damages
DNA -- but almost completely
absorbed by ozone
p 75
OZONE absorbs harmful UVC & most harmful UVB
p 75
GC Savvy Link : Sunscreen Topic
The Skin Care Scoop
http://fp.arizona.edu/kkh/nats101gc/sun_essentials.htm
Updated table:
Check the active ingredients:
• titanium dioxide
• zinc oxide
• avobenzone (also called butyl
methoxydibenzoylmethane)
• Ecamsule (mexoryl sx)
are the KEY ingredients authorized for use in U.S.
products that protect you from the entire UVA spectrum.
Therefore, if one of those isn't listed as an active
ingredient on the label, the product should not be used
for sun protection by anyone!

NEXT:
THE DESTRUCTION OF
STRATOSPHERIC
OZONE
> CFCs are photo-dissociated into
FREE CHLORINE ATOMS (Cl) and other
molecular fragments by UV rays
> Chlorine (and other gases such as
Nitric oxide, NO) act as catalysts in ozone
loss reactions
Stratospheric ozone under steady
state natural conditions
Ozone reservoir
The Chapman Mechansim
“balance”
is being disrupted by the
introduction of CFC's and
other similar gases into the
stratosphere:
Key Concept
Through chemical reactions:
 the chlorine removes ozone from
the stratosphere
 and also frees more chlorine
atoms to begin the process all over
again
CATALYST =
A compound that increases the rate of
a chemical reaction and is itself
unchanged by the reaction
Key Concept

Threat to stratospheric
ozone of CHLORINE was
recognized in mid-1970s
(in CFCs, or “FREON”)
CFC compounds
Chlorofluorocarbons
are unreactive at
Earth’s surface,
but if they get into the
stratosphere, they can be
broken down by high energy
UV radiation  leads to
release of highly reactive
CHLORINE atoms (Cl)
CFCs: Trends
FREON-11
FREON-12
Human-made --
didn’t exist
before 1950!
Montreal Protocol
signed in 1987
review
CFC’s & the CHLORINE
CATALYST
A single chlorine atom may
destroy hundreds of thousands of
ozone molecules during its
residence in the stratosphere!
[Go to movie clip]
This chemical theory of ozone destruction by
CFC’s was first proposed in 1974 – but no
observations existed!
(Atmospheric chemists Crutzen, Molina, Rowland
were later given Nobel prize for this theory)
Key Concept
Volcanic effects
Solar effects
Other theories to explain the hole
have included:
• solar variability (sunspot cycle)
• dynamical air motion
• volcanic eruptions Key Concept
Overall, O3 is
decreasing in the
STRATOSPHERE
OZONE & ERUPTIONS
Stratospheric ozone is destroyed by
photochemical reactions that take place
on the surfaces of the sulfate aerosols
Note drop in ozone
amounts right after
eruptions
p 71
CHAPTER 1
• Ground-based ozone measurements
since 1956. (British survey team)
• They observed a new trend of
decreasing ozone concentrations
beginning in 1977
• Didn’t believe their measurements &
delayed publication for several years
while rechecking data & instruments.
Finally published in 1985;
greeted with skepticism! 
DISCOVERY OF THE OZONE HOLE:
“A Misadventure of Science?”

Declining OZONE
CONCENTRATIONS
(in Dobson units)
1957-1986
Early data from ground
measurements of British
survey team
(over Antarctica)
CHAPTER 2
• Meanwhile, satellites had been launched to
observe ozone from above via the TOMS
instrument on the satellite

DISCOVERY OF
THE OZONE HOLE
(cont.)
• TOMS detected the
developing hole, but the
anomalously low readings
were rejected as “noise” by
the computer program set up
to process the data !!
1970
1996
1971 1972 1979
1994
1993
1992
Total Ozone in October (DU)
CHAPTER 3
• In 1986 Dr. Susan Soloman’s
expedition to Antarctica  identified
chlorine increase
• She devised the theory that correctly
explained the destruction of ozone by
chlorine compounds

DISCOVERY OF THE
OZONE HOLE
(cont.)
SGC
Fig 1.6
ClO (chlorine
monoxide) from
the chlorine
catalytic cycle =
THE evidence of
chemical
reactions
occurring in
hole region
during time of
greatest O3
depletion
(in September,
spring in Southern
Hemisphere)
p 74
To the South Pole
ANTARCTIC LAND MASS
Color
version
of SGC
Fig 1.6
Simultaneous measurements of ozone (O3) and
chlorine monoxide (ClO)

The chemical reaction theory –
catalyzed by chlorine from CFCs --
is almost universally accepted as
conclusive at present.
The prominent scientists involved
in developing the chemical
reaction theory were awarded the
Nobel Prize for Physics in 1995.
Key Concept
WHY ANTARCTICA?
The ozone "hole(s)" have a unique
REGIONALITY and SEASONALITY :
> it is most severe over
Antarctica in S.H. spring (Sep, Oct);
> a less severe depletion (not a
true hole) occurs over the Arctic in N.H.
spring (Feb, Mar)
Key Concept
The special conditions that make ozone
depletion most severe over polar regions
(esp. Antarctica) are:
(2) The presence of POLAR STRATOSPHERIC ICE
CLOUDS -- on the surfaces of these extremely cold
cloud particles certain chemical reactions are more
efficient and faster.
(1) the unique CIRCUMPOLAR
CIRCULATION PATTERN over Antarctica in
winter which isolates the stratosphere inside
a vortex and acts like a "containment vessel"
in which chemical reactions may occur in
near isolation;
ICE CLOUDS
Key Concept
[Go to movie clip]
POLAR
STRATOSPHERIC
CLOUDS OVER
ANTARCTICA
LAST INGREDIENT:
SUNLIGHT + UV PHOTONS
Only after well after
the June Solstice and
esp. the September
Equinox, does the
South Pole &
Antarctic Circle
receive sufficient
sunlight!
Sept
June
When did the Hole
begin forming?
Hole generally
defined as
< 290 DU
p 77
RATE OF OZONE DEPLETION
in DOBSON UNITS (DU)
Sketch in the 290 DU
threshold line:
~ 1969 to 1970
http://ozonewatch.gsfc.nasa.gov/
see also: http://macuv.gsfc.nasa.gov/
2009
Update of graphs on
p 77 in Class Notes
p 77
The value of 85 Dobson Units
on October 8, 2006 was the
second lowest ever recorded by
satellite measurements.
HOW DEEP DOES THE
HOLE GET?
The intensity of ozone depletion
varies from year to year.
2006 also saw the
second LARGEST
sustained ozone hole.
http://www.sciencedaily.com/releases/2006/10/061019162053.htm
Nearly ALL of the ozone in the
layer 8-13 miles above the Earth's
surface was destroyed!
In this critical layer, the instrument
measured a record low of only 1.2
DU!

http://toms.gsfc.nasa.gov/eptoms/dataqual/oz_hole_avg_area_v8.jpg
Over time, the AVERAGE SIZE OF THE HOLE
has gotten LARGER:

http://www.youtube.com/watch?v=qUf
VMogIdr8&feature=player_embedded
Recap:
The area of 29 million square kilometers (11.4
million square miles) on September 24, 2006 tied
the largest value (on September 9, 2000)
Sep 9, 2000 Sep 24, 2006
Here are some inhabitants with strong cause for
concern about the Ozone Hole!
But what about the rest of us?

HOLE IN OZONE LAYER
EXPOSED A CITY
THE ASSOCIATED PRESS 10-6-00
WELLINGTON, New Zealand –
“The hole in the ozone layer over
Antarctica stretched over a
Chilean city when it ballooned to
a record size last month, the first
time it has reached a population
center, scientists said yesterday.
. . .

In an Upside-Down World, Sunshine Is Shunned
(New York Times 12-27-2002)
“Previously, the hole had only
opened over Antarctica and the
surrounding ocean.

“Citing data from NASA,
atmospheric research scientist
Stephen Wood said the hole
covered 11.4 million square miles -
an area more than three times the
size of the United States - on Sept.
9 and 10.
“For those two days, the
hole extended over Punta
Arenas, a southern Chilean
city of about 120,000
people, exposing residents
to very high levels of
ultraviolet radiation.
“ . . . findings showed a city
being exposed to the ozone
hole for the first time.”

A "solar stoplight" in Punta
Arenas announces an orange
alert, the second highest of four
levels, and warns people to limit
their exposure to the sun
between noon and 3 p.m. to a
maximum of 21 minutes.
a woman and her child are bundled up
against the sun
> Decreases have been observed in
nearly all latitude zones:
(1.1 - 9% in S.H. & 1.1 - 3.7% in N.H.)
> Mid-latitude ozone has been decreasing by ~
4% per decade in both hemispheres, whereas
tropical ozone has remained more or less
constant.
Key Concept
What about other parts
of the globe?
http://www.theozonehole.com/arcticozone.htm
Stratospheric Atmospheric Circulation
Determines this Distribution
Ozone production highest in tropics but
stratospheric circulation
distributes it poleward

http://www.theozonehole.com/arcticozone.htm

Arctic ozone depletion also takes place!
There are concerns that an “Arctic
Ozone Hole” may develop that is similar
to the severe Antarctic Hole
“An Arctic Ozone Hole, if similar in size to the Antarctic Ozone
Hole, could expose over 700+ million people, wildlife and
plants to dangerous UV ray levels.
The likely hood of this happening seems inevitable based on
the deterioration of ozone layer caused by the effects of global
warming on the upper atmosphere.”
Very long residence time of CFCs!
p 78
Model results
based on more
recent
agreements:
Vienna 1995
&
Montreal (again)
1997
The world is
“making do” with
freon substitutes,
but some concern
over long-term
effects of
substitutes
remains . . .
p 78
> Ozone is increasing in the troposphere
due to car exhaust, etc (“bad ozone”), but
only at the rate of about 1% per year,
> hence stratospheric levels of “good
ozone” are going down at a rate faster
than ozone is being added in the
troposphere.
Key Concept
Why can’t we just ship the “bad ozone” in
the troposphere up to the stratosphere
to ‘fill the hole’?
THE OZONE DEPLETION STORY
TIES TOGETHER MANY OF THE
CONCEPTS YOU’VE LEARNED IN
THE COURSE THUS FAR:
> the nature of matter, e.g.,
chemical reactions and photon
interaction with atoms

> the electromagnetic spectrum
--especially the wavelengths of
UV radiation

> absorption curves,
especially the absorption curve
for ozone

> Effect of clouds -- in this case the
importance of Polar Stratospheric
Clouds (PSCs)
> Greenhouse gases (ozone is also a
greenhouse gas but this affects IR
radiation, not UV radiation)

> the vertical structure of the
atmosphere (troposphere,
stratosphere)

> the ever-changing nature of
science; early theory right for wrong
reason

> Preconceived
ideas
influencing
one’s
observations
. . . and the
surprise of
discovery!

http://www.theozonehole.com/discoverer.htm
http://www.youtube.com/watch?v=Dn3KvZ_Xyqs&eurl=ht
tp://www.theozonehole.com/discoverer.htm
The OZONE & THE
MONTREAL PROTOCOL
The Discover of the Ozone
Hole issues a warning
MOVIE TIME !
ENJOY YOUR VETERAN’S
DAY BREAK ON WED & I’LL
SEE YOU ON THURSDAY –
DON’T FORGET
Deliverable #1
or RQ-8

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Ozone Depletion Explained

  • 1. SIT ANYWHERE YOU LIKE TODAY! TODAY: TOPIC #14 OZONE DEPLETION Tuesday Nov 10th • GC SAVVY COMSUMER PROJECT: Deliverable #1 is due before MIDNIGHT TONIGHT! (go to D2L to find the link to submit it) • RQ-8 is DUE Thu Nov 12 (30 min before class) • Some class time will be provided on Thursday for your groups to strategize on your GROUP’s GC topic presentation.
  • 2. IMPORTANT GUIDELINES on the GC SAVVY COMSUMER PROJECT: Purpose of the assignment is to link the GLOBAL CHANGE TOPICS OF THIS CLASS with your everyday life – so your consumer product research / selection criteria MUST have a direct link to at least ONE of our CLASS TOPICS! e.g.: -Ecological Footprint / Carbon Footprint (food choices/ vegetarian diet, transport vs. local food) - Electromagnetic Spectrum & harmful UV radiation, ozone depletion issues - The balance between auto crashworthiness (Laws of Motion) and fuel economy (GH Gas Emissions) - Energy Efficiency ( solar, electronics w/ energy Star ratings) - Deforestation / Sustainability (paper products, recycling, etc.)
  • 3. Topic # 14 OZONE DEPLETION IN THE STRATOSPHERE see pp 75-79 in Class Notes
  • 4. “[ The Ozone Treaty is ] the first truly global treaty that offers protection to every single human being.” ~ Mostofa K. Tolba, Director of the UN Environment Programme
  • 6. Generally, the Self Tests have been very useful for me in this class. I like how they summarize the major points of each topic and the help they provide on the RQ’s. They also are a good reference to use while studying for tests.  To me, the self-tests are extremely useful. I love being able to read the question, my choices for an answer, and then automatically being able to learn whether or not I was correct. Not only do I like being able to see how I did answering the question, but there is an explanation as to why the answer is correct or incorrect, which is very very useful for studying! I’m very grateful! I think the self tests are very useful because they prepare you well for the Readiness quiz after you have read the material. I almost get a 5 every time because of these self tests. I am thankful for the help. SELF TEST BONUS POINT !!
  • 7. The real answer: The ozone hole is: -- a depletion of ozone in the lower stratosphere -- that has occurred with increasing severity each spring (since measurements begin in 1970s) NOTE: the “Key Concepts” are all provided on p 79
  • 8. OZONE STORY = A very interesting illustration of the scientific process! The THEORY that the ozone layer in the stratosphere might be damaged by human intervention PRECEDED the actual OBSERVATION of the ozone hole. Yet, when the hole WAS observed (via satellite) it was almost “missed” because it wasn’t expected . . . Key Concept But let’s begin with the stratospheric ozone layer itself . . . . . .
  • 9. WHERE IS THE OZONE LAYER? Stratosphere Ozone Concentration (ppm) SGC Fig. 3-11 
  • 10. OZONE: Sources Ozone is produced naturally in photochemical reactions in the stratospheric ozone layer --“good ozone” -- is decreasing! However, ozone has increased in troposphere due to photochemical smog reactions -- “bad ozone” review
  • 11. Here’s a different version of the figure  Shows 2 peaks, a major peak in O3 density in the stratosphere, a smaller secondary peak in the lower troposphere Ozone Density (1017 molecules / m3) p 76
  • 12.  22 km altitude peak  Bulk of ozone produced at ~ 25 km & drifts downward Another lesser peak at ground level First we’ll focus on the “GOOD” ozone located in the STRATOSPHERE (the ozone that is being depleted leading to an ozone “hole”)
  • 13. THE OZONE LAYER IN THE STRATOSPHERE -- WHY IT'S THERE Due to: the natural “Chapman Mechanism” (a series of photochemical reactions)
  • 14.  ozone is continuously produced and destroyed  through PHOTOCHEMICAL REACTIONS in the stratosphere  involves oxygen (O2), molecular oxygen (O), photons of UV radiation, and OZONE (O3). THE CHAPMAN MECHANISM (first proposed in 1930s) Key Concept
  • 15. O O O O O O O O O O O O O O + + The Chapman Mechanism p 75
  • 16. O O O O O O O O O O O O O O 
  • 17. The Chapman Mechanism (another view) [Go to movie clip] Ozone being formed naturally Ozone being destroyed naturally Ozone being destroyed naturally Ozone being formed naturally p 75
  • 18. In theory: a balance of ozone is established over time > prevents much of the harmful UV radiation from reaching the earth's surface. Leads to an “Equilibrium” or “Steady State” Key Concept
  • 19. STEADY STATE = a condition in which the STATE of a system component (e.g. reservoir) is CONSTANT over time. 
  • 20. Steady state can be achieved in a reservoir: a) if there are no inflows or outflows, or b) if the rate of inflow = the rate of outflow. Any imbalance in these rates leads to a change in the level of the reservoir. 
  • 21. FLOW DIAGRAM OF A STEADY STATE Reservoir of STRATOSPHERIC OZONE Inflow Ozone being formed via natural Chapman mechanism Outflow Ozone being destroyed via natural Chapman mechanism Stratospheric ozone under steady state natural conditions Ozone reservoir After an initial period of adjustment a steady state is reached  as a horizontal line 
  • 22. Review: Why stratospheric ozone is “Good”: p 75 Ozone has the property of being a very strong absorber of ultraviolet radiation  nearly total absorption of wavelengths less than 0.3 m Black areas = radiation absorbed  remember this figure?
  • 23. Circle the CORRECT completion to this sentence: The global change issue usually referred to as Stratospheric Ozone Depletion is related to the part of the absorption curve that is labeled ____. X or Y
  • 24. 1. . . . because X represents UV radiation being absorbed -- hence if ozone is depleted, MORE ultraviolet radiation will reach the Earth’s surface. 2. . . . because X represents terrestrial longwave radiation being absorbed -- and hence serves as a catalyst in the Chapman mechanism. 3. . . .because X represents easy transmission of wavelengths of terrestrial longwave radiation out to space which then disappear through the “atmospheric window” also known as the ozone hole. Ok, X is right, but Why?
  • 25. Ozone Density graph Temperature graph Now roughly sketch the temperature line from this graph onto the ozone graph First sketch in tropopause & stratopause p. 38 in Class Notes: p 76
  • 26. TEMPERATURE [ increases / decreases ] with increasing altitude in the stratosphere WHY??? p 76
  • 27. 1. It is the closest layer to the sun, hence it is closest to the solar “heat source.” 2. It receives large amounts of UV radiation from the sun PLUS it has a high concentration of ozone to absorb this UV. 3. It is the layer which contains most of the GH gases that absorb IR radiation emitted by the Earth’s surface. Why is there an increase in temperature with altitude in the STRATOSPHERE?
  • 28. What about the “BAD” ozone located in the troposphere?  Ozone has increased in troposphere due to photochemical smog reactions  “bad ozone”
  • 29. HEALTH AND ENVIRONMENTAL EFFECTS OF GROUND-LEVEL OZONE Why are We Concerned about Ground-Level Ozone?  Ozone is the prime ingredient of smog in our cities and other areas of the country. http://www.epa.gov/ttn/oarpg/naaqsfin/o3health.html 
  • 30.  When inhaled, even at very low levels, ozone can: • cause acute respiratory problems • aggravate asthma • cause significant temporary decreases in lung capacity • cause inflammation of lung tissue • lead to hospital admissions & emergency room visits • impair the body's immune system defenses http://www.epa.gov/ttn/oarpg/naaqsfin/o3health.html 
  • 31.  “BAD” OZONE Ground-level ozone is a form of pollution created when: nitrogen oxides in auto emissions + hydrocarbons from plant matter + solvents and gasoline fumes . . . . mix and bake in stagnant heat and sunlight! http://www.airinfonow.org/html/ozoneMC.html Tucson data
  • 32. ANOTHER LINK TO EVERYDAY LIFE: SUN SAFETY!
  • 36. Wavelength Range Name Biological Effect .32 to .4 m (320-400 nm) UVA (SPF doesn’t rate UVA protection!) once thought to be relatively harmless, BUT causes wrinkles, premature aging and associated sun-related skin damage; new research indicates possible skin cancer link .29 to .32 m (290-320 nm) UVB (see SPF for protection) harmful, causes sunburn, skin cancer, and other disorders .20 to .29 m (200 - 290 nm) UVC (almost completely absorbed by O3) extremely harmful, damages DNA -- but almost completely absorbed by ozone p 75
  • 37. OZONE absorbs harmful UVC & most harmful UVB p 75
  • 38. GC Savvy Link : Sunscreen Topic The Skin Care Scoop http://fp.arizona.edu/kkh/nats101gc/sun_essentials.htm Updated table:
  • 39. Check the active ingredients: • titanium dioxide • zinc oxide • avobenzone (also called butyl methoxydibenzoylmethane) • Ecamsule (mexoryl sx) are the KEY ingredients authorized for use in U.S. products that protect you from the entire UVA spectrum. Therefore, if one of those isn't listed as an active ingredient on the label, the product should not be used for sun protection by anyone! 
  • 41. > CFCs are photo-dissociated into FREE CHLORINE ATOMS (Cl) and other molecular fragments by UV rays > Chlorine (and other gases such as Nitric oxide, NO) act as catalysts in ozone loss reactions Stratospheric ozone under steady state natural conditions Ozone reservoir The Chapman Mechansim “balance” is being disrupted by the introduction of CFC's and other similar gases into the stratosphere: Key Concept
  • 42. Through chemical reactions:  the chlorine removes ozone from the stratosphere  and also frees more chlorine atoms to begin the process all over again CATALYST = A compound that increases the rate of a chemical reaction and is itself unchanged by the reaction Key Concept
  • 43.  Threat to stratospheric ozone of CHLORINE was recognized in mid-1970s (in CFCs, or “FREON”) CFC compounds Chlorofluorocarbons are unreactive at Earth’s surface, but if they get into the stratosphere, they can be broken down by high energy UV radiation  leads to release of highly reactive CHLORINE atoms (Cl)
  • 44. CFCs: Trends FREON-11 FREON-12 Human-made -- didn’t exist before 1950! Montreal Protocol signed in 1987 review
  • 45. CFC’s & the CHLORINE CATALYST A single chlorine atom may destroy hundreds of thousands of ozone molecules during its residence in the stratosphere! [Go to movie clip] This chemical theory of ozone destruction by CFC’s was first proposed in 1974 – but no observations existed! (Atmospheric chemists Crutzen, Molina, Rowland were later given Nobel prize for this theory) Key Concept
  • 46. Volcanic effects Solar effects Other theories to explain the hole have included: • solar variability (sunspot cycle) • dynamical air motion • volcanic eruptions Key Concept Overall, O3 is decreasing in the STRATOSPHERE
  • 47. OZONE & ERUPTIONS Stratospheric ozone is destroyed by photochemical reactions that take place on the surfaces of the sulfate aerosols Note drop in ozone amounts right after eruptions p 71
  • 48. CHAPTER 1 • Ground-based ozone measurements since 1956. (British survey team) • They observed a new trend of decreasing ozone concentrations beginning in 1977 • Didn’t believe their measurements & delayed publication for several years while rechecking data & instruments. Finally published in 1985; greeted with skepticism!  DISCOVERY OF THE OZONE HOLE: “A Misadventure of Science?”
  • 49.  Declining OZONE CONCENTRATIONS (in Dobson units) 1957-1986 Early data from ground measurements of British survey team (over Antarctica)
  • 50. CHAPTER 2 • Meanwhile, satellites had been launched to observe ozone from above via the TOMS instrument on the satellite  DISCOVERY OF THE OZONE HOLE (cont.) • TOMS detected the developing hole, but the anomalously low readings were rejected as “noise” by the computer program set up to process the data !! 1970 1996 1971 1972 1979 1994 1993 1992 Total Ozone in October (DU)
  • 51. CHAPTER 3 • In 1986 Dr. Susan Soloman’s expedition to Antarctica  identified chlorine increase • She devised the theory that correctly explained the destruction of ozone by chlorine compounds  DISCOVERY OF THE OZONE HOLE (cont.)
  • 52. SGC Fig 1.6 ClO (chlorine monoxide) from the chlorine catalytic cycle = THE evidence of chemical reactions occurring in hole region during time of greatest O3 depletion (in September, spring in Southern Hemisphere) p 74 To the South Pole ANTARCTIC LAND MASS
  • 53. Color version of SGC Fig 1.6 Simultaneous measurements of ozone (O3) and chlorine monoxide (ClO) 
  • 54. The chemical reaction theory – catalyzed by chlorine from CFCs -- is almost universally accepted as conclusive at present. The prominent scientists involved in developing the chemical reaction theory were awarded the Nobel Prize for Physics in 1995. Key Concept
  • 55. WHY ANTARCTICA? The ozone "hole(s)" have a unique REGIONALITY and SEASONALITY : > it is most severe over Antarctica in S.H. spring (Sep, Oct); > a less severe depletion (not a true hole) occurs over the Arctic in N.H. spring (Feb, Mar) Key Concept
  • 56. The special conditions that make ozone depletion most severe over polar regions (esp. Antarctica) are: (2) The presence of POLAR STRATOSPHERIC ICE CLOUDS -- on the surfaces of these extremely cold cloud particles certain chemical reactions are more efficient and faster. (1) the unique CIRCUMPOLAR CIRCULATION PATTERN over Antarctica in winter which isolates the stratosphere inside a vortex and acts like a "containment vessel" in which chemical reactions may occur in near isolation; ICE CLOUDS Key Concept
  • 57. [Go to movie clip] POLAR STRATOSPHERIC CLOUDS OVER ANTARCTICA
  • 58. LAST INGREDIENT: SUNLIGHT + UV PHOTONS Only after well after the June Solstice and esp. the September Equinox, does the South Pole & Antarctic Circle receive sufficient sunlight! Sept June
  • 59. When did the Hole begin forming? Hole generally defined as < 290 DU p 77 RATE OF OZONE DEPLETION in DOBSON UNITS (DU) Sketch in the 290 DU threshold line: ~ 1969 to 1970
  • 61. The value of 85 Dobson Units on October 8, 2006 was the second lowest ever recorded by satellite measurements. HOW DEEP DOES THE HOLE GET? The intensity of ozone depletion varies from year to year. 2006 also saw the second LARGEST sustained ozone hole. http://www.sciencedaily.com/releases/2006/10/061019162053.htm Nearly ALL of the ozone in the layer 8-13 miles above the Earth's surface was destroyed! In this critical layer, the instrument measured a record low of only 1.2 DU! 
  • 64. The area of 29 million square kilometers (11.4 million square miles) on September 24, 2006 tied the largest value (on September 9, 2000) Sep 9, 2000 Sep 24, 2006 Here are some inhabitants with strong cause for concern about the Ozone Hole! But what about the rest of us? 
  • 65. HOLE IN OZONE LAYER EXPOSED A CITY THE ASSOCIATED PRESS 10-6-00 WELLINGTON, New Zealand – “The hole in the ozone layer over Antarctica stretched over a Chilean city when it ballooned to a record size last month, the first time it has reached a population center, scientists said yesterday. . . .  In an Upside-Down World, Sunshine Is Shunned (New York Times 12-27-2002)
  • 66. “Previously, the hole had only opened over Antarctica and the surrounding ocean.  “Citing data from NASA, atmospheric research scientist Stephen Wood said the hole covered 11.4 million square miles - an area more than three times the size of the United States - on Sept. 9 and 10.
  • 67. “For those two days, the hole extended over Punta Arenas, a southern Chilean city of about 120,000 people, exposing residents to very high levels of ultraviolet radiation. “ . . . findings showed a city being exposed to the ozone hole for the first time.”  A "solar stoplight" in Punta Arenas announces an orange alert, the second highest of four levels, and warns people to limit their exposure to the sun between noon and 3 p.m. to a maximum of 21 minutes. a woman and her child are bundled up against the sun
  • 68. > Decreases have been observed in nearly all latitude zones: (1.1 - 9% in S.H. & 1.1 - 3.7% in N.H.) > Mid-latitude ozone has been decreasing by ~ 4% per decade in both hemispheres, whereas tropical ozone has remained more or less constant. Key Concept What about other parts of the globe? http://www.theozonehole.com/arcticozone.htm
  • 69. Stratospheric Atmospheric Circulation Determines this Distribution Ozone production highest in tropics but stratospheric circulation distributes it poleward 
  • 70. http://www.theozonehole.com/arcticozone.htm  Arctic ozone depletion also takes place! There are concerns that an “Arctic Ozone Hole” may develop that is similar to the severe Antarctic Hole “An Arctic Ozone Hole, if similar in size to the Antarctic Ozone Hole, could expose over 700+ million people, wildlife and plants to dangerous UV ray levels. The likely hood of this happening seems inevitable based on the deterioration of ozone layer caused by the effects of global warming on the upper atmosphere.”
  • 71. Very long residence time of CFCs! p 78
  • 72. Model results based on more recent agreements: Vienna 1995 & Montreal (again) 1997 The world is “making do” with freon substitutes, but some concern over long-term effects of substitutes remains . . . p 78
  • 73. > Ozone is increasing in the troposphere due to car exhaust, etc (“bad ozone”), but only at the rate of about 1% per year, > hence stratospheric levels of “good ozone” are going down at a rate faster than ozone is being added in the troposphere. Key Concept Why can’t we just ship the “bad ozone” in the troposphere up to the stratosphere to ‘fill the hole’?
  • 74. THE OZONE DEPLETION STORY TIES TOGETHER MANY OF THE CONCEPTS YOU’VE LEARNED IN THE COURSE THUS FAR: > the nature of matter, e.g., chemical reactions and photon interaction with atoms 
  • 75. > the electromagnetic spectrum --especially the wavelengths of UV radiation 
  • 76. > absorption curves, especially the absorption curve for ozone 
  • 77. > Effect of clouds -- in this case the importance of Polar Stratospheric Clouds (PSCs) > Greenhouse gases (ozone is also a greenhouse gas but this affects IR radiation, not UV radiation) 
  • 78. > the vertical structure of the atmosphere (troposphere, stratosphere) 
  • 79. > the ever-changing nature of science; early theory right for wrong reason 
  • 80. > Preconceived ideas influencing one’s observations . . . and the surprise of discovery! 
  • 81.
  • 83. MOVIE TIME ! ENJOY YOUR VETERAN’S DAY BREAK ON WED & I’LL SEE YOU ON THURSDAY – DON’T FORGET Deliverable #1 or RQ-8