6.2 Stratospheric Ozone.

Slides:



Advertisements
Similar presentations
Bell ringer.
Advertisements

By Narmada Harish & Daniel Cheng
Objectives Explain how the ozone layer shields the Earth from much of the sun’s harmful radiation. Explain how chlorofluorocarbons damage the ozone layer.
5.6 Ozone Depletion By: Aditi.
The Ozone Layer. * What is the stratospheric ozone? The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and.
Alejandro Martínez Erick Castillo Giuliana Villegas
Ozone is made of three oxygen atoms - O 3 Ozone. OZONE – A Greenhouse gas Greenhouse gas. Near ground it is a nasty pollution In the stratosphere it protects.
Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with.
1 “The greenhouse effect itself is simple enough to understand and is not in any real dispute. What is in dispute is its magnitude over the coming century,
THE OZONE LAYER What is it? Where is it?
Atmosphere and Climate ChangeSection 2 Bellringer.
Recall – quick questions 1.In which 2 layers of the atmosphere is ozone found? 2.Where is it considered “good” and “bad”? Why? 3.What happens to the structure.
Objectives Explain how the ozone layer shields Earth from much of the sun’s harmful radiation. Explain how chlorofluorocarbons damage the ozone layer.
Chapter 15 Air Pollution and Stratospheric Ozone Depletion.
Day one Chapter 13 Atmosphere and Climate Change
Atmosphere and Climate ChangeSection 2 Section 2: The Ozone Shield Preview Bellringer Objectives The Ozone Shield Chemicals That Cause Ozone Depletion.
Section  Area in the stratosphere where ozone is highly concentrated  Ozone: 3 atoms of oxygen (O3)  Absorbs most of the harmful ultraviolet.
Stratospheric Ozone Depletion
Atmosphere Review Composition of air Nitrogen (78%) Oxygen (21%)
Atmosphere and Climate ChangeSection 2 The Ozone (O 3 ) Shield Ozone layer: layer of the atmosphere at an altitude of 15 to 40 km where ozone absorbs UV.
International Environmental Policy: Controlling Ozone Depletion.
Ozone O3O3 Ozone Depletion Ozone (O 3 ) –Absorbs harmful UV radiation from sun ozone is produced during lightning storms Chlorofluorocarbons (CFC’s)
5.6 Depletion of Stratospheric Ozone. Depletion of Ozone.
Depletion of Stratospheric Ozone. Composition of the Atmosphere Chemical Composition: Nitrogen (N 2 )- 78% Oxygen (O 2 )- 21% Carbon Dioxide (CO 2.
Atmosphere and Climate ChangeSection 2 Section 2: The Ozone Shield Preview Bellringer Objectives The Ozone Shield Chemicals That Cause Ozone Depletion.
13-2 The Ozone Shield Page 335.
SCIENCE OF OZONE LAYER DEPLETION 12 th - 13 th March, 2007 (JAIPUR) By Rashid Ayub (MIS Coordinator-PMU)
Air Pollution and Stratospheric Ozone Depletion
POLLUTION MANAGEMENT 5.6 Depletion of stratospheric ozone.
Objectives Explain how the ozone layer shields the Earth from much of the sun’s harmful radiation. Explain how chlorofluorocarbons damage the ozone layer.
Chapter 13, Section 2: the ozone shield Standards: SEV4f ATMOSPHERE & CLIMATE CHANGE.
ENVIRONMENTAL SCIENCE Chapter 13 Atmosphere and Climate Change 13.2 The Ozone Shield.
Depletion of the ozone layer Not the Greenhouse effect.
DAY ONE Chapter 13 Atmosphere and Climate Change Section 2: The Ozone Shield.
T HE T HIN B LUE B LANKET Environmental Science 2.1.
Depletion of stratospheric Ozone Urban Air pollution Acid Deposition Depletion of stratospheric Ozone Urban Air pollution Acid Deposition.
Stratospheric Ozone (O 3 ) Formation and Depletion History of problem and solution Tie to Climate Change.
6.2 Stratospheric Ozone.
Stratospheric Ozone Holy Ozone!.
Day one Chapter 13 Atmosphere and Climate Change
PRESENTERS: Maria Malik Umm e hani Hussnain Ali.
Section 13-2 The Ozone Shield.
Day one Chapter 13 Atmosphere and Climate Change
“ A growing hole of problems”
Classroom Catalyst.
Quick review of atmosphere layers
Ozone and CFCs Intro.
Environmental Science Witt
THE OZONE LAYER What is it? Where is it?
Atmosphere Composition of air Nitrogen (78%) Oxygen (21%)
Ozone Prevents UV-B radiation from reaching the Earth
Stratospheric Ozone.
Ozone Depletion.
Day one Chapter 13 Atmosphere and Climate Change
Section 2: The Ozone Shield
Day one Chapter 13 Atmosphere and Climate Change
Day one Chapter 13 Atmosphere and Climate Change
THE OZONE LAYER What is it? Where is it?
Section 2: The Ozone Shield
Day one Chapter 13 Atmosphere and Climate Change
Air Pollution and Stratospheric Ozone Depletion
Day one Chapter 13 Atmosphere and Climate Change
Atmosphere and Climate Change
Day one Chapter 13 Atmosphere and Climate Change
DAY ONE Chapter 13 Atmosphere and Climate Change
OZONE LAYER AND PESTICIDES A PRESENTATION BY ALLAH DAD KHAN.
Assessment statements Depletion of Stratospheric Ozone
Day one Chapter 13 Atmosphere and Climate Change
The ozone hole has only ever been observed to be well south of the Australian mainland and Tasmania. In fact, during springtime, when the hole is in existence,
Section 2: The Ozone Shield
Presentation transcript:

6.2 Stratospheric Ozone

Atmosphere

Stratosphere 12-50 km thick Temperature increases with altitude (gets warmer!) Horizontal winds (jet stream) Contains ozone layer

Ozone 3 oxygen molecules

Ozone – O3 Dynamic equilibria Balance between two ongoing processes UV radiation passing through the Earth’s upper atmosphere is absorbed by the formation and destruction of ozone.

Ozone UV (ultraviolet) radiation is absorbed during the formation and destruction of ozone into oxygen (O2)

Ozone and UV light Allows UVa and UVb through, but blocks UVc waves   Allows UVa and UVb through, but blocks UVc waves UVa - causes wrinkles UVb - causes skin cancer UVc - worst one because of damage to organisms/tissues

UV radiation also affects other living organisms Damage to photosynthetic organisms. Especially phytoplankton – basis of many aquatic food webs.

Beneficial Effects of UV In animals stimulates the production of Vit D. Treat psoriasis and vitiligo (skin diseases) Steriliser, water purifier Forensics, lighting, lasers

Damage to the Ozone

CFCs are usually very stable CFCs are usually very stable. However, in the high stratosphere the UV radiation breaks them down releasing free chlorine atoms (chlorine is very reactive)

HOGS (Halogenated Organic Gases) HOG’s are usually stable but break down into halogen atoms (F, Cl, Br, I, At) which are highly reactive Ex. (CFC = chlorofluorocarbon Cl and F are halogens Organic = contains carbon

Depletion of Ozone

Damage to the ozone ODS (Ozone-depleting substance) Substance Use/source Notes Chlorofluorocarbons (CFCs or freons) Hydrochlorofluorocarbon (HCFCs) Halons Methyl bromide Nitrogen Oxides (NO, NO2, N2O, NOx)

Sources of CFC’s fire extinguishers, refrigerators, AC units

Sources of CFC’s fire extinguishers, refrigerators, AC units

Pollution Management Strategies

Reducing ODS Apply the “Replace, regulate and restore” model of pollution management to ODS. Strategy Example of action Altering the human activity producing pollution (replace). Regulate and reduce the pollutants at the point of emission. Clean up and restoration

Pollution Management of CFC’s and HOGS Reduce-Regulate-Restore model Reduce: Replace CFC’s with CO2, propane, or air Replace aerosol propellants Replace methylbromide pesticides with something other than GHG’s Don’t use aerosol hair products or deodorant

Pollution Management of CFC’s and HOGS Regulate: Require a switch to HCFC’s because they don’t persist as long in the atmosphere; (They are still harmful to the ozone layer…just less so) Create laws to require refrigerators returned to manufacturers to recover harmful materials inside Capture CFC’s from scrap cars AC units

Pollution Management of CFC’s and HOGS Restore: Remove chlorine from the stratosphere or add ozone (not exactly feasible!) Ozone layer is slowly replenishing itself as long as we continue the ban

National and International Organizations

National and International Organizations UNEP (United Nations Environmental Programme) Montreal Protocol 1987

National and International Organizations UNEP (United Nations Environmental Programme) Key role in: Providing information Creating and evaluating international agreements Protection of stratospheric ozone

National and International Organizations Montreal Protocol 1987 International agreements on the reduction of ODS use. National laws and regulations aimed at reducing consumption of ODS (CFCs in particular)

The Montreal Protocol 1987 This protocol is very significant for a number of reasons: Best example of international cooperation on an environmental issue. An example of the precautionary principle in science-based decision making. Experts from many different fields coming together to research a problem and find solutions. The first to recognise that different countries could phase-out ODS chemicals at different times depending on their economic status. The first with regulations that were carefully monitored. Precautionary principle - in environmental matters, the theory that if the effects of a product or action are unknown, then the product should not be used or the action should not be taken

Hair Bands Ruined the Ozone Poison 1983… so much hairspray