Polar Ozone: Stratosphere- Troposphere Coupling and recent Changes 16.01.08 Proseminar Presentation Techniques Axel Behrendt.

Slides:



Advertisements
Similar presentations
Atmosphere Layers separated by temperature variations.
Advertisements

Climate Models.
I/1 Overview: Atmospheric transport and ozone chemistry SS2008 Learning more about variability of atmospheric ozone related to transport and chemistry.
Annular Modes of Extra- tropical Circulation Judith Perlwitz CIRES-CDC, University of Colorado.
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Ozone and the Ozone Hole Heather Raven & Stefanie Spayd.
Climate Change.
Stratospheric Chemistry EPS March – 04 April 2011 Polar Stratospheric Clouds.
Lecture 2: Composition & Structure of the Atmosphere (Ch1) Composition (continued) Vertical structure of the atmosphere Hurricane Florence, a problem for.
Bay Area Earth Science Institute (BAESI)
Radiative Forcing of Ozone
CHAPMAN MECHANISM FOR STRATOSPHERIC OZONE (1930) O O 3 O2O2 slow fast Odd oxygen family [O x ] = [O 3 ] + [O] R2 R3 R4 R1.
National Oceanic and Atmospheric Administration Geophysical Fluid Dynamics Laboratory Princeton, NJ Evolution of Stratospheric.
THE OZONE LAYER What is it? Where is it?
Influence of the sun variability and other natural and anthropogenic forcings on the climate with a global climate chemistry model Martin Schraner Polyproject.
Ozone & Greenhouse Effect. What is Ozone? Ozone is a molecule that occurs in the Stratosphere Ozone absorbs harmful UV rays from the sun O 3 + uv O 2.
Greenhouse Effect - Natural Heating of Earth’s surface by certain atmospheric gases.
Energy in the Atmosphere
24.1 The Atmosphere. 1. Define the atmosphere… 2. What molecule has the highest concentration in the atmosphere? ( oxygen, Carbon dioxide, nitrogen?)
QUESTIONS Based on the major source of OH described last class where do you expect OH formation to be high? 2. The  Chapman mechanism includes a fifth.
 DMS 6 th Grade Science.  Gravity pulls gas molecules in atmosphere toward Earth, causing air pressure  As altitude ↑, air pressure ↓
Lecture 16 Observations of climate change Feedback mechanisms Air pollution The stratospheric ozone hole Changing land surfaces Greenhouse gases and global.
Sensitivity of Methane Lifetime to Sulfate Geoengineering: Results from the Geoengineering Model Intercomparison Project (GeoMIP) Giovanni Pitari V. Aquila,
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.
 Mostly made of nitrogen gas & oxygen gas Gases that absorb and re-emit infrared radiation  Water vapour  Carbon dioxide  Methane  Nitrous oxide.
QUESTIONS 1.Based on the major source of OH described last class where do you expect OH formation to be high? 2.Why don’t reactions of hydrocarbons deplete.
NEXT Characteristics of the Atmosphere Atmospheric Heating Global and Local Winds Air Pollution Random Facts
Analysis of a simulation with prognostic ozone in ARPEGE-Climat Jean-François Royer, Hubert Teysseidre, Hervé Douville, Sophie Tyteca Meteo-France,
Climate change and stratosphere-troposphere coupling: Key questions Eugene Cordero, Nathan Gillett, Michael Sigmond, Shigeo Yoden.
Climate Change. Greenhouse Effect Earth would be too cold to live on without the Greenhouse Effect Greenhouse gases are carbon dioxide, water vapor, methane,
21.3 Climate Change. Natural Processes That Change Climate Volcanic eruptions The presence of volcanic ash, dust, & aerosols in the air increases the.
24 Global Ecology. Global Biogeochemical Cycles Atmospheric CO 2 affects pH of the oceans by diffusing in and forming carbonic acid.
ATMOSPHERE BY: Alexis A- Sweizy Carr.
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.
7. Ozone hole 1)Structure of the ozone layer 2) Chemistry of the natural ozone layer 3)Recent changes to the ozone layer 4)Effects of Chlorine on global.
Carbon Dioxide CO 2 RF = 1.66 W/m 2. Methane CH 4 RF = 0.48 W/m 2.
By: Justin Woodfin. The Basics The atmosphere is a mixture of gases that surrounds the earth. The atmosphere contains the oxygen we need to breathe it.
Past and Future Changes in Southern Hemisphere Tropospheric Circulation and the Impact of Stratospheric Chemistry-Climate Coupling Collaborators: Steven.
Sensitivity of Antarctic climate to the distribution of ozone depletion Nathan Gillett, University of East Anglia Sarah Keeley, University of East Anglia.
How do Long-Term Changes in the Stratosphere Affect the Troposphere?
Recent Trend of Stratospheric Water Vapor and Its Impacts Steve Rieck, Ning Shen, Gill-Ran Jeong EAS 6410 Team Project Apr
Chapter 3 Introduction to the Atmosphere.  Supplies oxygen for humans & animals  Supplies carbon dioxide (CO 2 ) for plants  Helps maintain water supply.
THE ATMOSPHERE. aTMOSPHERIC pRESSURE Air Pressure- the measure of the force with which the air molecules push on a surface. Air pressure changes throughout.
IVb/1 IV. Stratospheric ozone chemistry 1.Basic concepts of atmospheric chemistry 2.Ozone chemistry and ozone distribution 3.Sources and distribution of.
I/1 Atmospheric transport and ozone chemistry Lecture SS 2008 Mark Weber S4350 Tel Lecture material of today:
Jim Angell’s contributions to understanding the QBO.
Dynamical Impacts of Antarctic Stratospheric Ozone Depletion on the Extratropical Circulation of the Southern Hemisphere Kevin M. Grise David W.J. Thompson.
1. The atmosphere 2 © Zanichelli editore 2015 Characteristics of the atmosphere 3 © Zanichelli editore 2015.
Trends in lower stratosphere Jean-François Lamarque (NCAR and NOAA) and Susan Solomon (NOAA)
Chapter 4 Section 4 Global Changes in the Atmosphere.
If it were not for greenhouse gases trapping heat in the atmosphere, the Earth would be a very cold place. Greenhouse gases keep the Earth warm through.
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Land, Water, and Air Resources Chapter Global Changes in the Atmosphere.
1 Can variations in the tropical convection and circulation play a role in the variability of the Antarctic ozone? Leila M. V. Carvalho 1,2 and Charles.
Climate Change and Ozone Loss Chapter 21. Key Concepts  Changes in Earth’s climate over time  Factors affecting climate  Possible effects of global.
Atmosphere and Climate Change Chapter 13 Environmental Science.
CHAPTER 13 – ATMOSPHERE AND CLIMATE CHANGE Section 3a – Climate Change.
Chapter 22: Earth’s Atmosphere
Climate Dynamics 11:670:461 Alan Robock
Weakened QBO Due to Stronger Mean Tropical Upwelling
Interannual Variations in Stratospheric Water Vapor
Group 5472 Kolchanov S Khusainov R
Structure of the atmosphere
Atmosphere.
The Atmosphere.
b. Composition of the Atmosphere
Objective 11: I can define ozone layer and greenhouse effect
GLOBAL CLIMATE CHANGE AN OVERVIEW.
THE ATMOSPHERE I CAN EXPLAIN HOW HEAT IS TRANSFERRED IN THE ATMOSPHERE. I CAN DESCRIBE CONDUCTION. I CAN DESCRIBE CONVECTION. I CAN DESCRIBE RADIATION.
Presentation transcript:

Polar Ozone: Stratosphere- Troposphere Coupling and recent Changes Proseminar Presentation Techniques Axel Behrendt

Contents Part A: Stratosphere-Troposphere Coupling Part B: Recent Polar Ozone Changes 1.Radiation 2.Dynamics 3.Composition of the Stratosphere 4.Impact on Climate 1.Antarctic Ozone Hole Polar Ozone Trends 1/13

1. Radiation Part A: Stratosphere-Troposphere Coupling Increase of Greenhouse Gases 2/ Gas Phase Reactions slow down More PSCs

1. Radiation 11-Year Sun-Cycle 3/13 Part A: Stratosphere-Troposphere Coupling Meridional temperature gradient is modified Brewer Dobson Circu- lation is modified

2. Dynamics Stratosphere-Troposphere-ExchangeBrewer Dobson Circulation 4/13 Part A: Stratosphere-Troposphere Coupling

2. Dynamics Quasi Biennial Oscillation 5/13 Part A: Stratosphere-Troposphere Coupling

2. Dynamics Chemical Composition of the Troposphere: Long lived species: CH 4, N 2 O, CFCs, COS, … Short lived species: SO 2 DMS 6/13 Part A: Stratosphere-Troposphere Coupling

3. Composition of the Stratosphere Stratospheric Aerosols (SO 2, COS from volcanoes) 7/13 Part A: Stratosphere-Troposphere Coupling Stratospheric Water Vapor From: WMO-Report 2007

4. Impact on Climate 500 hPa Geopotential Height [m] Surface Temp. [K] and Winds 8/13 Part A: Stratosphere-Troposphere Coupling From: WMO-Report 2007

Part B: Recent Polar Ozone Changes 9/13

Part B: Recent Polar Ozone Changes 1. The Antarctic Ozone Hole /13 From: WMO-Report 2007

2. Polar Ozone Trends Antarctic: 11/13 Part B: Recent Polar Ozone Changes

2. Polar Ozone Trends 12/13 Part B: Recent Polar Ozone Changes

Thanks for your attention !! 13/13