5.6 Depletion of Stratospheric Ozone. Depletion of Ozone.

Slides:



Advertisements
Similar presentations
Bell ringer.
Advertisements

5.6 Ozone Depletion By: Aditi.
Water and Weather Chapter Five: Earth’s Atmosphere 5.1 The Atmosphere 5.2 Layers of the Atmosphere 5.3 Earth is Just Right.
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
The Atmosphere.
Depletion of Ozone Composition of Atmosphere Troposphere 0-12km thick; 75% of all gases in atmosphere; All weather happens here; Temperature falls with.
Atmosphere and Climate ChangeSection 2 Bellringer.
Earth’s First Atmosphere 1. NH 3 2. CH 4 3. H 2 O * How did the first atmosphere change into the second atmosphere? Earth’s Second Atmosphere 1. N 2 2.
Objectives Explain how the ozone layer shields Earth from much of the sun’s harmful radiation. Explain how chlorofluorocarbons damage the ozone layer.
I. Earth’s Past Atmospheres: 1.) Volcanoes and lava covered earth which gave off NH 3, CH 4, which enters earth’s first atmosphere. 3.) The suns rays.
Atmosphere. Layers of the Atmosphere The atmosphere has four layers: –Thermosphere –Mesosphere –Stratosphere –Troposphere.
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
Do Now: We use models to describe or represent things 1. Describe what you see in the beaker/container on the counter. 2. What do you think this beaker.
OZONE LAYER & CFC’S. Understanding Stratospheric Ozone Discovered in 1839 by Christian Schonbein Pale blue, unstable, made up of 3 oxygen atoms Found.
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.
Ozone Layer O 3 Absorbs the sun’s UV radiation Stratosphere 20-50km above the Earth’s surface.
Question.1 Discuss the problems associated with the use of CFCs. by.bashar & philip.
Characteristics of the atmosphere lecture 22.1b. Composition Gases in air: Gases in air: N 78% O 2 21% Argon 0.93% CO 2.035% Thickness: 400 mi. from surface.
International Environmental Policy: Controlling Ozone Depletion.
Atmosphere and Climate ChangeSection 2 Section 2: The Ozone Shield Preview Bellringer Objectives The Ozone Shield Chemicals That Cause Ozone Depletion.
OZONE LAYER oOzone layer is made up from ozone molecule. oAn ozone molecules is made up of three oxygen atom bound together. oIts located 19-48km above.
DO NOW The Atmosphere Hill Science 6. The Atmosphere 1. Which layer is the densest layer of the atmosphere containing almost 90% of the atmosphere’s mass?
Atmosphere.
Topic 5.6 Depletion of Stratospheric Ozone. Ozone Overview The ozone layer is the part of the Earth's atmosphere which contains relatively high concentrations.
ATMOSPHERE REVIEW DRILL: DESPITE LAWS PASSED TO REDUCE AIR POLLUTION WHY DOES THE PROBLEM STILL EXIST? OBJECTIVE: SWBAT IDENTIFY KEY CONCEPTS OF THE ATMOSPHERE.
Earth’s Unique Atmosphere 1. Magnetic Field: a layer of electrical charges that protects Earth from solar winds and cosmic rays Caused by: the liquid.
Bellwork March 1, 2007 Define the following words: Page 434 Define the following words: Page 434 –Atmosphere –Troposphere –Ionosphere –Ultraviolet Radiation.
OZONE DEPLETION & CLIMATE CHANGE (Ch 20). ELECTROMAGNETIC SPECTRUM.
AtmosphereAtmosphere. Importance: 1) balance between heat absorbed from Sun and amount that escapes back (extreme temperatures) 2) protects Earth from.
OZONE DEPLETION IN THE STRATOSPHERE
Layers of Earth’s atmosphere. How was the atmosphere formed? Atmosphere has changed (evolved) over time. Gases are held near the surface by gravity. Earth’s.
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.
The Earth’s…. The planet earth has a mixture of gases surrounding it called the atmosphere.
Earth’s Atmosphere intro intro. Atmospheric Composition Gas% Nitrogen78% Oxygen21% Argon0.9% Carbon Dioxide0.04% Other Gases, Dust and Water Vapor 0.06%
Layers of the Atmosphere. What is the Atmosphere? A mixture of gases and other materials that surround the Earth Nitrogen 78% Oxygen 21% Argon 0.93% Carbon.
Exosphere  Uppermost layer  Beyond this lies space.
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.
Unit 7 – The Atmosphere and Water
Composition of atmosphere
Our Atmosphere. Important to Earth . Provides Protection,
OBJECTIVES: a. describe the layers of the atmosphere. b
The Atmosphere Copyright © Houghton Mifflin Harcourt Publishing Company.
Quick review of atmosphere layers
The Atmosphere.
Atmosphere Composition of air Nitrogen (78%) Oxygen (21%)
Layers of Earth’s atmosphere
Ozone Prevents UV-B radiation from reaching the Earth
Unit 6: The Atmosphere.
Ozone Depletion.
Atmosphere Basics.
Layers of Earth’s atmosphere
Layers of Earth’s atmosphere
ATMOSPHERE.
Layers of the atmosphere
6.2 Stratospheric Ozone.
Assessment statements Depletion of Stratospheric Ozone
Layers of Earth’s atmosphere
Presentation transcript:

5.6 Depletion of Stratospheric Ozone

Depletion of Ozone

Composition of Atmosphere

Troposphere 0-12km 75% of all gases in atmosphere; All weather happens here; Temperature falls with altitude

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

Mesosphere 50-80km Temperature falls with altitude Meteor showers happen here

Thermosphere km Aurora borealis and aurora australis Ionosphere here (reflects radio waves for communications) Very hot (2000 C+) !

Exosphere Outermost layer of earth’s atmosphere 550km+ above earth’s surface Satellites orbit here

Ozone 3 oxygen molecules UV (ultraviolet) radiation is absorbed during the formation and destruction of ozone into oxygen (O 2 )

Ozone and UV light 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 O2 + O + UV → O3 The energy provided by incoming UV light changes O2 → O3

Ozone and 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

Process of Ozone Depletion How ozone is depleted by CFC’s: 1. UV radiation breaks off a chlorine atom from a CFC molecule. 2. The chlorine atom attacks an ozone molecule (O 3 ), breaking it apart and destroying the ozone. 3. The result is an ordinary oxygen molecule (O 2 ) and a chlorine monoxide molecule (ClO). 4. The chlorine monoxide molecule (ClO) is attacked by a free oxygen atom releasing the chlorine atom and forming an ordinary oxygen molecule (O 2 ). 5. The chlorine atom is now free to attack and destroy another ozone molecule (O 3 ). One chlorine atom can repeat this destructive cycle thousands of times. S ources of HOG’s - fire extinguishers, refrigerators, AC units

UV light and ozone

UV radiation on Life Reacts with melanin in skin to cause sunburn & skin cancer Overexposure degrades immune system (but how?)

UV radiation and life Required for production of vitamin D (GOOD!) Interferes with photosynthesis in producers (esp. phytoplankton) Zooplankton then gain less energy from phytoplankton, and food chain suffers (i.e. productivity decreases)

Methods of reducing HOGS Replace CFC’s with CO 2, propane, or air Don’t use aerosol hair products or deodorant Create laws to require refrigerators returned to manufacturers to recover harmful materials inside Capture CFC’s from scrap cars AC units 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 Policies UNEP (United Nations Environment Program) forges agreements on: ITIHC (International Trade in Harmful Chemicals) air pollution contamination of international waterways provide information to countries and public on disadvantages of pollution 1987 Montreal Protocol international agreement on the emission of ozone-depleting substances froze production and consumption of CFC’s with goal of zero production by year 2000 LEDC’s granted a longer time to implement the treaty China and India have not met their quotas under the MP because of their rapid economic growth and high demand for refrigeration & AC’s good example of a successful international cooperative effort to alter human impact on the environment

Hair Bands Ruined the Ozone Poison 1983… so much hairspray