1 EFFECTS OF ANTHROPOGENIC EMISSIONS ON STRATOSPHERIC OZONE NWADIKE ONYINYECHUKWU BY.

Slides:



Advertisements
Similar presentations
Volcanoes Large volcanic eruptions with high SO2 content can release SO2 into the stratosphere. This SO2 eventually combined with water vapor to make.
Advertisements

Earths Climate System Dr. R. M. MacKay. Natural and Anthropogenic Climate Forcing.
HFCs: A Critical Link in Protecting Climate and the Ozone Layer A. R. Ravishankara Guus Velders Melanie Miller Mario Molina Steering committee headed by.
I/1 Overview: Atmospheric transport and ozone chemistry SS2008 Learning more about variability of atmospheric ozone related to transport and chemistry.
3 April 2012, Bonn, Germany Limitations of Single-Basket Trading: Lessons from the Montreal Protocol for Climate Policy John S. Daniel National Oceanic.
Ozone and the Ozone Hole Heather Raven & Stefanie Spayd.
A science/policy success story: The world avoided by the Montreal Protocol Greg Bodeker Presented at A Silver lining Celebrating 25 years of the Montreal.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
 The atmosphere is a layer of gases that surround the Earth.  These layers differ in temperature, in density, and in the relative amounts of the different.
Bay Area Earth Science Institute (BAESI)
What are aerosols ? Aerosol is a collection of particles suspended in the air, they range in size from 0.01 microns to several tens of microns.
Radiative Forcing of Ozone
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
STRATOSPHERIC CHEMISTRY. TOPICS FOR TODAY 1.Review of stratospheric chemistry 2.Recent trends in stratospheric ozone and forcing 3.How will stratospheric.
A Changing Climate: Past, Present and Future AT 351 Lecture 13 Dec 7, 2009.
MET 12 Global Climate Change – Lecture 8
Earth’s Changing Environment Lecture 5 Depletion of the Ozone Layer.
Climate ‘fix’ could deplete ozone
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Atmosphere and Climate Change
Newly detected ozone-depleting substances in the atmosphere SAP Presentation OEWG, Paris, July 2014.
The Greenhouse effect Is a natural process necessary for sustaining life on earth Is a natural process necessary for sustaining life on earth Is produced.
Ozone Layer in the 21 st Century Swagath Navin Manohar.
Human Influence on Weather/Climate Chapter 18 material.
Links between ozone and climate J. A. Pyle Centre for Atmospheric Science, Dept of Chemistry University of Cambridge Co-chair, SAP 7th ORM, Geneva, 19.
Greenhouse Effect and Global Warming Greenhouse Effect Key Factors Earth-Sun Temperature Differences Greenhouse Gas Concentrations The atmosphere is.
Chapter 19 Global Change. Global change-Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures.
1 Assessment of the Stratospheric Ozone Layer: Past and Future (Karma of and Nirvana for O 3 ) A.R. (Ravi) Ravishankara NOAA, Earth System Research Laboratory.
Natural and Anthropogenic Drivers of Arctic Climate Change Gavin Schmidt NASA GISS and Columbia University Jim Hansen, Drew Shindell, David Rind, Ron Miller.
PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
21.3 Climate Change. Natural Processes That Change Climate Volcanic eruptions The presence of volcanic ash, dust, & aerosols in the air increases the.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 5: Atmospheric Structure / Earth System Don Wuebbles Department of Atmospheric Sciences.
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
Question.1 Discuss the problems associated with the use of CFCs. by.bashar & philip.
1 Global Changes in the Atmosphere Global Warming and Ozone Depletion msnbcmedia.msn.com/j/msnbc/Components/Photos/...
2. Climate: “average” weather conditions, but the average doesn’t stay steady. I.e. Ice ages, El Niño, etc. 1. Weather: state of the atmosphere at a given.
Q14 Do changes in the Sun and volcanic eruptions affect the ozone layer? Claudia Mignani.
Essential Questions: 1) What role have humans played in the destruction of the Ozone Layer? 2) Why should humans be concerned about the destruction of.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 11 Radiative Forcing Eugene Cordero San Jose State University Outline  GHG/Aerosols.
Fundamentals Atmosphere Climate Variation Greenhouse Effect Climate Drivers Carbon Cycle Energy Balance System Inertia Geologic time Causes of Climate.
Chapter 23 The Atmosphere, Climate, and Global Warming.
The sun is the primary source of Energy to Earth’s climate system.
1 Ozone depletion: Misconceptions Misconceptions Meteorology 10 De Anza College.
1May 14, 2014 Uncertainties in projections of ozone- depleting substances and alternatives Guus Velders The Netherlands (RIVM)
The Basic Research Model Models/Theory NWP GCM/CSMs Process Mods. Observations Soundings Satellites Surface Obs. Predictions Boundary Conditions Initial.
AAAHHHHH!!!!. Climate Change Climate Physical properties of the troposphere of an area based on analysis of its weather records over a long period Two.
I. I.Climate Change – Greenhouse Gases A. A.Background Greenhouse Effect Gases absorb heat (not light) Natural Greenhouse Effect Mean planetary temperature.
Stratospheric Ozone Brent Greenhalgh and Carrie Welker Reviews in Earth Science Oct. 4, 2011 September 17, 1979 October 1, 2010 (NASA, )
The Greenhouse effect Is a natural process necessary for sustaining life on earth Is a natural process necessary for sustaining life on earth Is produced.
1 Ozone module prepared by Eugene C. Cordero Lesson 4 "Ozone Depletion: The future?"
Links between ozone and climate 9 th ORM Geneva, 14 May 2014 SAP Co-chairs Ayité-Lô Ajavon (Togo) Paul Newman (USA) John Pyle (UK) A.R. Ravishankara (USA)
Climate Change: Impacts and Responses Topic 2: The Earth's Climate System 1.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Aim: How have air pollutants affected the atmosphere?
World Regional Geography Unit I: Introduction to World Regional Geography Lesson 4: Global Environmental Problems.
Global Change.
The Greenhouse Effect.
Greenhouse Effect and Global Warming
A. R. Ravishankara, John S. Daniel, Robert W. Portmann (2009)
Science Thoughts 10/23 What is an atmosphere? An atmosphere is a layer of gases surrounding a planet or other material body, that is held in place by the.
Chapter 19 Global Change.
Is Global Warming the Biggest Issue of Our time?
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. 4 ways the atmosphere affects.
The Atmosphere.
b. Composition of the Atmosphere
Climate Change: Fitting the pieces together
Greenhouse Gases and Climate Change
Intro to Climate Change
Essential Question: How do volcanoes affect the climate
Presentation transcript:

1 EFFECTS OF ANTHROPOGENIC EMISSIONS ON STRATOSPHERIC OZONE NWADIKE ONYINYECHUKWU BY

Nwadike Onyinye28/11/20072 Outline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/20073 Outiline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/20074 The climate system and interaction Mark Weber, 2004 Glossary: Luft=air, Eis=ice, Wechselwirkung=interaction, Kreisläufe=cycles, kurzwellig=shortwave, langwellig=long wave, Schnee=snow, Weltraum=space,Strömung=current, Seen=lakes, Flüsse=rivers, Niederschlag=precipitation, Zuläufe=streams, Wolken=clouds

Nwadike Onyinye28/11/20075 Outline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/20076 Atmospheric Forcing of Climate Change: Anthropogenic effect +VE Forcing, warming of the earth by WMGHG conc. -VE Forcing, ozone depletion in stratosphere, cooling of earth. Primary forcing mechanism affecting stratospheric climate change WMO, 2006

Nwadike Onyinye28/11/20077 The Roles of Trace Gases in the Stratosphere Willams Brunne, 1991

Nwadike Onyinye28/11/20078 Sources,Reservior, and Reactive Species for the Chemical Species Willams Brunne, 1991

Nwadike Onyinye28/11/20079 Outiline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/ Stratospheric Ozone Production WMO, 2006

Nwadike Onyinye28/11/ CHAPMAN CYCLE

Nwadike Onyinye28/11/ OZONE DESTRUCTION CYCLE WMO, 2006

Nwadike Onyinye28/11/ Principal Steps in the Depletion of Stratospheric Ozone WMO, 2006

Nwadike Onyinye28/11/ Polar Ozone Depletion Hofmann et al. 1994

Nwadike Onyinye28/11/ Outline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/ Effect of Volcanism WMO, 2006  Large volcanic eruptions decreases solar transmission to Earth’s surface.  Increase in ozone depletion by the emitted particles.

Nwadike Onyinye28/11/ Outline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/ Global Ozone: Recovery Stages WMO, 2006

Nwadike Onyinye28/11/ Outline  Introduction  Atmospheric Forcing of Climate Change: Anthropogenic effect  Ozone Production and Loss Processes  Effect of Volcanic Eruption  Effect of Montreal Protocol on Ozone Recovery  Conclusion / Summary

Nwadike Onyinye28/11/ Conclusions/Summary  CFCs account for large ozone destruction because they have longer lifetime  Human activites contribute to indirect radiative forcing effect  Volcanic eruptions is a natural process that enhance Ozone depletion but cannot be predicted.  Montreal Protocol may lead to a complete ozone recovery by the year 2100

THANKS FOR YOUR ATTENTION ANY QUESTIONS?