Strategies for containing climate change below dangerous levels. V. Ramanathan Scripps Institution of Oceanography, UCSD Georgia Tech, Jan 20, 2010
|
|
- Kerrie Amelia Gibson
- 6 years ago
- Views:
Transcription
1 Strategies for containing climate change below dangerous levels V. Ramanathan Scripps Institution of Oceanography, UCSD Georgia Tech, Jan 20, 2010
2 Sources of greenhouse Gases and Aerosols in Brown Clouds. Ramanathan 2007
3
4 Source: NOAA/ESRL Global Monitoring Division 2006 { The Keeling Curve}
5 Ramanathan 2007
6 PUBLISHED 1971 Oh, Mother earth, ocean-girdled and mountainbreasted, pardon me for trampling on you Sanskrit Prayer
7 1975 Abstract. The infrared bands of chlorofluorocarbons and chlorocarbons enhance the atmospheric greenhouse effect. This enhancement may lead to an appreciable increase in the global surface temperature if the atmospheric concentrations of these compounds reach values of the order of 2 parts per billion. One molecule of CFC has the same greenhouse effect as the addition of more than molecules of Carbon Dioxide to the Atmosphere
8 The Non CO2 trace gases contribute as much as CO2 to the increase in atmospheric Greenhouse effect: Ramanathan et al, JGR, 1983
9 Source: Updated: PLENARY, IPCC 2007
10 Earth Radiation Budget Experiment: { Joined Team in 1975} Ramanathan, Barkstrom and Harrison, Physics Today, 1989
11 The Water Vapor Feedback Temp dependence of Saturation vapor pressure: σt 4 e s : e -5400/T στ 4 d lne dt s 5400 = T
12
13 1980
14 Unequivocal Warming of the Planet: IPCC, 2001 & 2007
15 Global Radiative Forcing due to GHGs : IPCC 2007 A F 3 3 Wm 2 RC: Ramanathan & Carmichael, 2008
16 Ramanathan and Feng, 2008 IPCC AR4 (2007) Concludes: For a CO 2 doubling, the most likely climate sensitivity is 3 C warming with a 90% confidence interval of 2 to C For doubling of CO 2, TOA forcing is : 3.7 Wm 2 So it takes about 1.25 Wm 2 (3.7/3) to warm the planet by 1 0 C The GHGs so far have added 3 Wm 2 forcing The committed (or the inevitable) warming is C
17 Dangerous Anthropogenic Interference with Climate (PNAS, 2008) Committed warming derived from IPCC Forcing & IPCC climate sensitivity
18 Ramanathan-2007 Los Angeles Dec 27, 2002
19 Indian Ocean Experiment (INDOEX): Lead Agencies: NSF; ISRO; Max Planck Co-Chair: Ramanathan & Crutzen Ramanathan et al; J Gephys Res; 2001
20 Global Dimming: Direct Evidence Ash Black carbon 7% 11% Dust 12% MISS Organics 2% 17% a-salt & NO 3-11% K + 2% 26% 12% NH 4 + SO 4 = Meywerk and Ramanathan, 2000 Ramanathan et al, 2001
21 Aerosol Induced Dimming: 2002 {A Synthesis of ground, aircraft and satellite observations} Chung, Ramanathan, Kim, Podgorny,2005 Greenhouse Forcing = 3 W/m**2 Brown Cloud Masking= -1.5 (+-50%) W/m**2
22 Ramanathan et al, Nature, 2007.
23 ABCs surround Back Scattering (Cooling) the Himalayas NASA, CALYPSO LIDAR Ramanathan et al, 2007 ABC-Pyramid Station; Base Camp Mt Everest; Fuzzi et al 08
24 Major Rainfall Shifts during the last 50 Years Chung and Ramanathan 2006 Observed Trends in Summer Rainfall: 1950 to 2002 N-S Shift in Asian rainfall The Weakening Indian Monsoon The Sahelian Drought
25
26 What is being considered in Intl Negotiations 2007 Carbon emission: 8.5 Gtons/Yr as CO 2 At fixed emission, by 2030 we will add: If we reduce emission by 50% by 2030, We will still be adding : 108 Gtons 81 Gtons Fossil Fuel Em ission (GtC/y Emissions
27 Even with 50% reductions by 2050, CO2 will Increase to 440 PPM; Commit another 1 C warming concentration(ppm) emission(gt/year) CO2 reductions have to be complemented with Reductions in short-lived non-co2 warming agents
28 Non-CO 2 climate warmers Contribution to 2005 forcing relative to CO 2 (1.66 Wm -2 ) Ref: Forster, Ramaswamy et al, WG1-AR4, IPCC, 2007 Greenhouse Gases Ozone (troposphere) : 20% Methane : 30% Halocarbons : 20% Particles (Aerosols) Black Carbon : 27% to 55% * (soot/smoke) Total Non-CO 2 : 97% to 125% All numbers except the red are IPCC values; Long lived N 2 O not included * Ramanathan & Carmichael; 2008
29 Pathway to limiting global warming to 2 0 C I. Reduce CO 2 by 50% before 2050 II. Reduce short lived warming agents: Roughly 30% in 30 Years Black Carbon (<2 weeks); Ozone (< 2 months); Methane (<15 years) HFCs & HCFCs (<15 years) Buy about 30 years time: to develop transformational technologies for a massive thinning of the GHGs blanket: Zero emission of CO 2
30 Helping communities implement practices that mitigate global warming, and gathering the data needed to improve the health of the planet.
31 The Challenge Biomass Cooking and Global Warming Economic conditions force more than 3 billion of people to burn biomass such as wood, charcoal, and dung to cook their food. These fires emit black carbon (a major component of soot), ozone- producing gases, methane and numerous other gases and particles that pollute indoor and outdoor air. Moreover, since wood is one of the primary fuels used in burning of these fires, biomass cooking also leads to deforestation. Since trees store carbon, such deforestation in turn leads to greater atmospheric concentration of carbon dioxide (CO 2 ).
32 Smoke and BC have Major Impacts on Health; Water Security and Food Security Indoor Smoke contributes as much as 2/3 of BC outdoors Indoor smoke contributes as much as 500,000 deaths annually in India Greatest advantage for Policy Actions 1. Short Lived in the air ( about a week or less) 2. Immediate response to mitigation laws 3. Response felt locally by improved air quality 4. Will reduce fatalities due to indoor and outdoor air pollution
33 Target mitigation (Surya) a) Baseline BC AOD for 2004/05 Rural Cooking Biogas plants converts organic waste into gas Ramanathan and Balakrishnan, 2007 Ramanathan and Carmichael, 2008 b) BC AOD without biofuels Parabolic solar cooker
34 Project Surya s Objectives 1. Introduce cleaner-cooking technologies. 2. Gather data on climate and health outcomes. 3. Use the data to scale up and expand the project.
35 The Data Needed to Make a Difference Project Surya is more than a cleaner-cooking program. It is a scientific intervention. What distinguishes Project Surya from numerous other cleaner-cooking projects is its scope and evaluation. The multi-disciplinary team will undertake the most comprehensive and rigorous scientific evaluation to date on the efficacy of reducing biomass-fueled cooking on climate warming. Positive results could lead to its replication in other soot-producing regions such as China and Africa, saving millions of lives.
36 Technology: Documenting the Mitigation Ramanathan and Thomas, 2009 Phase 1: 5000 to households
37 Surya: Pilot Village : Khairatpur, Indo Gangetic Plains, N India Rehman, Siva, Ramana, Kar & Ramanathan, 2010
38 0:58 1:58 2:58 3:58 4:58 5:58 6:58 7:58 8:58 9:58 10:58 11:58 12:58 13:58 14:58 15:58 16:58 17:58 18:58 19:58 20:58 21:58 22:58 23:58 Preliminary Black Carbon Data in Pilot Village: Rehman, Siva, Ramana, Kar and Ramanathan, Mean Kairatpur BC (Oct 15 - Nov 18) Mean Jagdishpur BC (Nov 19 - Nov 26) Morning Cooking BC Concentartaion μg m Evening Cooking
39 From personal observations to global patterns (Nithya Ramanathan and Deborah Estrin, CENS, UCLA) + Time spent in kitchen cooking Activities outdoors (e.g. walk, run, drive) Estimates pollution exposure Map of exposure worldwide NASA
40
41 Evaluating Health Impacts Epidemiologists at Sri Ramachandra University will employ the cellphone tool. They will also undertake surveys and professional observation to evaluate Project Surya s impacts on the health of women and childrenvillagers.
42 Bottom of the Pyramid The four billion people who live on less than $2 per day constitute the bottom of the economic and energy pyramid. CAN WE STEER THEM INTO A SUSTAINABLE NON-FOSSIL FUEL PATHWAY AND ENABLE THEM TO CLIMB TO THE TOP OF THE ENERGY PYRAMID?
Helping communities implement practices that mitigate global warming, and gathering the data needed to improve the health of the planet.
Helping communities implement practices that mitigate global warming, and gathering the data needed to improve the health of the planet. Table of Contents EXECUTIVE SUMMARY Objectives.........3 How Surya
More informationproject surya MITIGATION OF GLOBAL AND REGIONAL CLIMATE CHANGE AND HEALTH IMPACT
project surya MITIGATION OF GLOBAL AND REGIONAL CLIMATE CHANGE AND HEALTH IMPACT July 10, 2010 EXPECTED OUTCOME REGIONAL Increase food and water supply, decrease mountain-glacier melt, decrease deforesta
More informationAir Pollution and the Climate System: Sustainability Now and Later
Air Pollution and the Climate System: Sustainability Now and Later Tami C. Bond Department of Civil & Environmental Engineering University of Illinois at Urbana-Champaign ISTC Seminar Series October 13,
More informationThe Fifth Assessment: A Discussion of the IPCC Working Group 1 AR5 Report
The Fifth Assessment: A Discussion of the IPCC Working Group 1 AR5 Report Prof. Chris E. Forest The Pennsylvania State University (ceforest@psu.edu) Lead Author - Chapter 9 - Evaluation of Climate Models!
More informationENVIS- IITM NEWSLETTER The Air Quality: A Global Challenge
ENVIS- IITM NEWSLETTER The Air Quality: A Global Challenge GLOBAL WARMING Editorial Prof. B.N. Goswami (Director, IITM, Pune) Dr. G. Beig (ENVIS Co-ordinetor) Ms. Neha S. Parkhi (Program Officer) Mr. Rajnikant
More informationGlobal Warming Science Solar Radiation
SUN Ozone and Oxygen absorb 190-290 nm. Latent heat from the surface (evaporation/ condensation) Global Warming Science Solar Radiation Turbulent heat from the surface (convection) Some infrared radiation
More informationGREENHOUSE GASES 3/14/2016. Water Vapor, CO 2, CFCs, Methane and NO x all absorb radiation Water vapor and CO 2 are the primary greenhouse gases
GREENHOUSE EFFECT The earth is like a greenhouse The atmosphere acts like the glass which lets the sun s rays pass through. The earth absorbs this as heat energy and keeps it in, only letting a little
More informationEnvironmental Impacts of. Energy Production
CH2356 Energy Engineering Environmental Impacts of Energy Production Dr. M. Subramanian Associate Professor Department of Chemical Engineering Sri Sivasubramaniya Nadar College of Engineering Kalavakkam
More informationTOPIC # 16 GLOBAL WARMING & ANTHROPOGENIC FORCING
TOPIC # 16 GLOBAL WARMING & ANTHROPOGENIC FORCING TODAY s 3 KEY CONCEPTS: Carbon / Forests / Deforestation Computer Model Evidence for Anthropogenic GW Forcing Tying it all together w/ RADIATIVE FORCING
More informationAtmosphere, the Water Cycle and Climate Change
Atmosphere, the Water Cycle and Climate Change OCN 623 Chemical Oceanography 16 April 2013 (Based on previous lectures by Barry Huebert) 2013 F.J. Sansone 1. The water cycle Outline 2. Climate and climate-change
More informationThe Chemistry of Climate Change. Reading: Chapter 8 Environmental Chemistry, G. W. vanloon. S. J. Duffy
The Chemistry of Climate Change Reading: Chapter 8 Environmental Chemistry, G. W. vanloon. S. J. Duffy The Science of Global Climate There's a lot of differing data, but as far as I can gather, over the
More informationBLACK CARBON RESEARCH INITIATIVE NATIONAL CARBONACEOUS AEROSOLS PROGRAM (NCAP)
BLACK CARBON RESEARCH INITIATIVE NATIONAL CARBONACEOUS AEROSOLS PROGRAM (NCAP) J.Srinivasan Divecha Centre for Climate Change Indian Institute of Science, Bangalore Particles of solid or liquid phase suspended
More informationClimate Change: What do we know and what do we guess?
What do we know and what do we guess? Manfred Grasserbauer * Vienna University of Technology * Director Institute for Environment and Sustainability, Joint Research Centre, European Commission (Ispra)
More informationIntroduction to the Role of Tropospheric Ozone and Arctic Climate. Ellen Baum May 8, 2008
Introduction to the Role of Tropospheric Ozone and Arctic Climate Ellen Baum May 8, 2008 There is a significant global role for tropospheric ozone and climate 1.4 Temperature impact from CO2 compared to
More informationAir Transportation: Emissions and Effects
Air Transportation: Emissions and Effects Joyce E. Penner University of Michigan Report Co-ordinator: IPCC Special Report on Aviation and the Global Atmosphere Presentation to the First Regional Symposium
More informationOVERVIEW AND INTRO TO CLIMATE SCIENCE MIT SUMMER HSSP, 2016 WEEK 1
OVERVIEW AND INTRO TO CLIMATE SCIENCE MIT SUMMER HSSP, 2016 WEEK 1 COURSE OVERVIEW THIS IS GOING TO BE FUN (I HOPE ) JOSH S BACKGROUND MIT: 2 nd Year Ph.D. Student Researching Atmospheric Chemistry U.C.
More informationClimate Change. Some solar radiation is reflected by Earth and the atmosphere. Earth s Surface
Q& A n The Basics of Greenhouse gases affect Earth s energy balance and climate The Sun serves as the primary energy source for Earth s climate. Some of the incoming sunlight is reflected directly back
More informationChapter 11: Atmosphere
To get you thinking This is our atmosphere. All life on Earth exists within this tiny protective blanket. Why is the atmosphere important to us? What do you think it does for us? Chapter 11: Atmosphere
More informationEarth s energy balance and the greenhouse effect
Earth s energy balance and the greenhouse effect Average incident solar radiation 342 W/m 2 Reflection to space by atmosphere, clouds, and earth surface 102 W/m 2 Infrared radiation emitted to space 240
More informationANNOUNCEMENTS: I-4 LESSON 4 on Intro to Climate Modeling is due TONIGHT by 11:59 pm
Thursday Nov 20th Topic #13 GLOBAL WARMING & ANTHROPOGENIC FORCING (cont.) SIT ANYWHERE TODAY! But pick up an INDEX CARD when you come it! ANNOUNCEMENTS: I-4 LESSON 4 on Intro to Climate Modeling is due
More informationLecture 2: Greenhouse Gases - Basic Background on Atmosphere - GHG Emission and Concentration Rise - California Regulation (AB32)
Lecture 2: Greenhouse Gases - Basic Background on Atmosphere - GHG Emission and Concentration Rise - California Regulation (AB32) METR 113/ENVS 113 Spring Semester 2011 February 15, 2011 Suggested Reading
More informationGlobal Climate Change: What the Future Holds, and What We Can Do About It
Global Climate Change: What the Future Holds, and What We Can Do About It Dr. David Karowe Professor, Department of Biological Sciences Schedule of Topics September 29: Recent climate change (Dave Karowe)
More informationIntroduction. Introduction. Introduction. Outline Last IPCC report : 2001 Last IPCC report :
Introduction Greenhouse Gases & Climate Change Laurent Bopp LSCE, Paris When did the story start? ¾1827 Fourier hypothesizes greenhouse effect ¾1860 Tyndal identifies CO2 and water vapor as heat trapping
More informationScientific Foundation of Climate Change. Human Responsibility for Climate Change
Scientific Foundation of Climate Change EOH 468 CSU Northridge Spring 2010 Peter Bellin, CIH, Ph.D. 1 Human Responsibility for Climate Change The IPCC finds that it is very likely that emissions of heat-trapping
More informationChapter 19: Global Change
1 Summary Of the Case Study Polar Bear population in the Antarctic going down because temperatures are going up and melting the caps. Polar bears are losing their habitat, they also can t get their food
More informationClimate Change and Ozone Loss
Climate Change and Ozone Loss During the past 900,000 years, the earth has undergone a series of cold glacial periods followed by warmer interglacial periods. The past 10,000 years has been an interglacial
More information1 Characteristics of the Atmosphere
CHAPTER 22 1 Characteristics of the Atmosphere SECTION The Atmosphere KEY IDEAS As you read this section, keep these questions in mind: What are the layers of Earth s atmosphere? How has Earth s atmosphere
More informationHimalayan-Tibetan Glaciers and Snowpack System: Multiple Destabilizing Influences
Fate of Mountain Glaciers in the Anthropocene Pontifical Academy of Sciences, Scripta Varia 118, 2013 www.pas.va/content/dam/accademia/pdf/sv118/sv118-ramanathan.pdf Himalayan-Tibetan Glaciers and Snowpack
More informationThe Greenhouse Effect
Name: #: Date: 5.8 The Greenhouse Effect The greenhouse effect traps heat in the atmosphere. This helps the Earth remain warm enough for humans. Without the greenhouse effect, human would not be able to
More informationClimate: Earth s Dynamic Equilibrium
Climate: Earth s Dynamic Equilibrium review session CCIU April 30, 2016 High-school standard HS-ESS2-4 focuses on the role energy flows play in Earth s climate HS-ESS2-4 Use a model to describe how variations
More informationGlobal Climate Change
Global Climate Change Devizes & District U3A, 24 th November 2015 Prof. Richard Allan, Department of Meteorology University of Reading Why does Earth s climate change? Earth s Climate has always been changing
More informationHow is the atmosphere different from outer space? a mixture of gases that surrounds the Earth
Chapter 15 Atmosphere Section 1 Objectives Describe the composition of Earth's atmosphere. Explain why air pressure changes with altitude. Explain how air temperature changes with atmospheric composition.
More informationTuesday Dec 2nd TOPIC # 13 Global Warming Wrap Up TOPIC #14 IMPACTS & ISSUES
Tuesday Dec 2nd TOPIC # 13 Global Warming Wrap Up TOPIC #14 IMPACTS & ISSUES SIT WITH YOUR GROUP TODAY ANNOUNCEMENTS: LINKING-TO-LIFE PROJECT PART A Your Ecological Footprint DUE in class TODAY! PART B
More informationConcept Paper. Asian Brown Clouds. DRAFT 1.1 May Air Pollution in the Indo-Asia-Pacific Region: Impact on Climate and the Environment
Concept Paper on Asian Brown Clouds Air Pollution in the Indo-Asia-Pacific Region: Impact on Climate and the Environment Integration of Science, Impact Assessment, Policymaking and Regional Capacity Building
More informationEnergy, Greenhouse Gases and the Carbon Cycle
Energy, Greenhouse Gases and the Carbon Cycle David Allen Gertz Regents Professor in Chemical Engineering, and Director, Center for Energy and Environmental Resources Concepts for today Greenhouse Effect
More informationTHE ANTHROPOCENE: THE CURRENT HUMAN-DOMINATED GEOLOGICAL ERA
Paths of Discovery Pontifical Academy of Sciences, Acta 18, Vatican City 2006 www.pas.va/content/dam/accademia/pdf/acta18/acta18-crutzen.pdf THE ANTHROPOCENE: THE CURRENT HUMAN-DOMINATED GEOLOGICAL ERA
More informationWhat Exactly is a Greenhouse Gas?
1 What Exactly is a Greenhouse Gas? You may have stood in a greenhouse and felt the heat, but what do greenhouse gases have to do with greenhouses? A greenhouse gas is any gas that absorbs and re-emits
More informationINTRODUCTION TO CLIMATE CHANGE SCIENCE AND IMPACTS ON URBAN AREAS. Febrauary16, 2015 TERI University, New Delhi
INTRODUCTION TO CLIMATE CHANGE SCIENCE AND IMPACTS ON URBAN AREAS Febrauary16, 2015 TERI University, New Delhi Aim of the lecture To understand relationship between greenhouse gases and climate change
More informationInterconnections between Air Pollution, Climate Change and Health
Interconnections between Air Pollution, Climate Change and Health Denise Mauzerall Princeton University National Academies Institute of Medicine San Francisco, CA September 10, 2007 Air Pollution Adversely
More informationUnderstanding the Causes of Global Climate Change
FACT SHEET I: Attribution Environment Understanding the Causes of Global Climate Change Average air temperatures at the Earth s surface have increased by approximately 0.6 o C (1 o F) over the 20 th century.
More informationUnderstanding how carbon dioxide emissions from human activity contribute to global climate change MYLES ALLEN Environmental Change Institute, School
Understanding how carbon dioxide emissions from human activity contribute to global climate change MYLES ALLEN Environmental Change Institute, School of Geography and the Environment & Department of Physics
More informationGLOBAL CLIMATE CHANGE
1 GLOBAL CLIMATE CHANGE From About Transportation and Climate Change (Source; Volpe center for Climate Change and Environmental forecasting, http://climate.volpe.dot.gov/trans.html Greenhouse effect has
More informationChapter 20 Air Pollution
Chapter 20 Air Pollution Overview of Chapter 20 Atmosphere as a Resource Types and Sources of Air Pollution Effects of Air Pollution Controlling Air Pollution in the US Ozone Depletion in the Stratosphere
More informationGlobal Warming Potentials in AR4. V. Ramaswamy. NOAA/ Geophysical Fluid Dynamics Laboratory, Princeton University
Global Warming Potentials in AR4 V. Ramaswamy NOAA/ Geophysical Fluid Dynamics Laboratory, Princeton University GWP Definition Defined as the ratio of the time-integrated radiative forcing from the instantaneous
More informationGreenhouse Effect. The Greenhouse Effect
Greenhouse Effect The Greenhouse Effect Greenhouse gases let short-wavelength radiation come into the Earth s atmosphere from the sun. However, they absorb and re-radiate Earth s long-wavelength radiation
More informationOverview of Chapter 19
19 Air Pollution Overview of Chapter 19 Atmosphere as a Resource Types and Sources of Air Pollution Effects of Air Pollution Controlling Air Pollution in the US Ozone Depletion in the Stratosphere Acid
More informationGLOBAL WARMING IS HAPPENING GLOBAL WARMING WILL BE VERY HARD TO STOP (By John B. Wheeler, member Potomac River Association)
GLOBAL WARMING IS HAPPENING GLOBAL WARMING WILL BE VERY HARD TO STOP (By John B. Wheeler, member Potomac River Association) READ ON AND SEE WHY YOU NEED TO BE WORRIED The Outline of what follows: 1 The
More informationGlobal Warming: What is the role of aerosol?
Global Warming: What is the role of aerosol? Barbara Wyslouzil, Sept. 10 2007 Outline Aerosols 101 The greenhouse effect Global temperature records The global warming problem How do aerosols play a role
More informationCurrent understanding of global climate change and of its possible impacts on agriculture. Maurizio Sciortino.
Current understanding of global climate change and of its possible impacts on agriculture Maurizio Sciortino maurizio.sciortino@enea.it Outline 1. Scientific understanding of climate change The greenhouse
More informationUN Climate Council Words in red are defined in vocabulary section (pg. 9)
UN Climate Council Words in red are defined in vocabulary section (pg. 9) To minimize the negative effects of global climate change, scientists have advocated for action to limit global warming to no more
More informationClimate Change: Global and Australian perspectives
Climate Change: Global and Australian perspectives Michael Raupach Centre for Australian Weather and Climate Research ESSP Global Carbon Project with Pep Canadell Thanks: GCP colleagues, CSIRO colleagues,
More informationOzone and trace gases in India: Effects of transport and emissions. Shyam Lal Physical Research Laboratory, Ahmedabad
Ozone and trace gases in India: Effects of transport and emissions Shyam Lal Physical Research Laboratory, Ahmedabad Second Workshop on Atmospheric Composition and the Asian Monsoon (ACAM), 8-10 June,
More informationGrade 10 Academic Science Climate Change Unit Test
Grade 10 Academic Science Climate Change Unit Test Part A - Multiple Choice: Circle the most correct answer. 1. What is the difference between weather and climate? a. Weather deals with wind and precipitation;
More informationHow things work college course/cumulative global warming exam/testbank
How things work college course/cumulative global warming exam/testbank From Wikiversity Contents 1 GlobalWarmingCumulative 1.1 GlobalWarmingCumulative v1s1 1.1.1 Key to GlobalWarmingCumulative v1s1 1.2
More informationClimate Change Vocabulary Global Challenges for the 21 st Century Tony Del Vecchio, M.Ed. Atmosphere
Atmosphere The mixture of gases surrounding the Earth. The Earth's atmosphere consists of about 79.1% nitrogen (by volume), 20.9% oxygen, 0.036% carbon dioxide and trace amounts of other gases. The atmosphere
More informationIntroduction to Climate Change. Rodel D. Lasco Professor University of the Philippines
RD Lasco 1 Introduction to Climate Change Rodel D. Lasco Professor University of the Philippines Outline The climate system What is climate change? Evidence for climate change Predicted change in climate
More informationChapter 2. Climate Change: Scientific Basis
a. The Greenhouse Effect Chapter 2 Climate Change: Scientific Basis Climate scientists have clearly established that: The Earth s atmosphere is like a greenhouse, reflecting some of the sun s harmful rays
More informationReducing Black Carbon Emissions from Open Burning: A Co-benefit of Landfill Methane Recovery
Reducing Black Carbon Emissions from Open Burning: A Co-benefit of Landfill Methane Recovery Nimmi Damodaran Joseph Donahue Inc., Washington DC Multiple Cobenefits of Landfill Methane Recovery Climate
More informationAir Pollution. Asian Brown Cloud. Developed Countries have reduced emissions recently
Study Questions 1. Compare and contrast primary vs. secondary pollutants, giving examples of each. 2. Compare and contrast indoor vs. outdoor pollution, listing specific examples and sources of each. 3.
More informationDr David Karoly School of Meteorology
Global warming: Is it real? Does it matter for a chemical engineer? Dr David Karoly School of Meteorology Email: dkaroly@ou.edu Recent global warming quotes Senator James Inhofe (R, Oklahoma), Chair, Senate
More informationSession 14 Unit VI CLIMATIC CHANGE AND GLOBAL WARMING
Session 14 Unit VI CLIMATIC CHANGE AND GLOBAL WARMING Dr. H.S. Ramesh Professor of Environmental Engineering S.J. College of Engineering, Mysore 570 006 Carbon di-oxide is a natural constituent of atmosphere,
More informationClimate Change Frequently Asked Questions Scrambled Information Source: EPA Climate Change FAQ
Climate Change Frequently Asked Questions Scrambled Information Source: EPA Climate Change FAQ Instructions: The questions and answers below have been scrambled. Cut the answers and questions apart. Separate
More informationClimate change What lies in the future? The Big Bang, the LHC and the God Particle
Climate change What lies in the future? The Big Bang, the LHC and the God Particle Cormac O Raifeartaigh (WIT) Cormac O Rafferty (WIT) Overview I Global warming Multiple lines of evidence II Natural climate
More informationConclusions of the IPCC Working Group I Fifth Assessment Report, AR4, SREX and SRREN
Conclusions of the IPCC Working Group I Fifth Assessment Report, AR4, SREX and SRREN R. K. Pachauri 11 November 2013 Warsaw, Poland Chairman, Intergovernmental Panel on Climate Change 1 Problems cannot
More informationIn 2011 burning of fossil fuels provided 83% of mankind s energy resource while nuclear electric power provided 9%, and renewable energy 8% (1).
Hierarchy of Global Energy Sources and Related Risks John Bushell January 2015 johnbushell@jbvm.com.au Abstract This paper reviews future energy resource options required to provide mankind with the energy
More information1. The diagram below shows a greenhouse.
1. The diagram below shows a greenhouse. 5. A gradual increase in atmospheric carbon dioxide would warm Earth s because carbon dioxide is a A) poor reflector of ultraviolet radiation B) good reflector
More informationClimate Change: Implications for Nebraska. Donald A. Wilhite School of Natural Resources University of Nebraska- Lincoln
Climate Change: Implications for Nebraska Donald A. Wilhite School of Natural Resources University of Nebraska- Lincoln The Politics of Climate Change Sen. Jim Inhofe (R-Okla.) has, once and for all, disproven
More informationName Date Class. This section describes Earth s atmosphere, or the layer of gases that surrounds the planet.
The Atmosphere Name Date Class The Atmosphere Guided Reading and Study The Air Around You This section describes Earth s atmosphere, or the layer of gases that surrounds the planet. Use Target Reading
More informationLocal and Global Impacts of Climate Change: Predictions of the 5th IPCC Report
Local and Global Impacts of Climate Change: Predictions of the 5th IPCC Report Peter Schlosser Department of Earth and Environmental Sciences and Department of Earth and Environmental Engineering The Earth
More informationGlobal warming: Evidence, risks and mitigation options (or: Why global warming is an energy issue) Filippo Giorgi Abdus Salam ICTP, Trieste
Global warming: Evidence, risks and mitigation options (or: Why global warming is an energy issue) Filippo Giorgi Abdus Salam ICTP, Trieste Four frequent questions Is global warming happening? (If yes)
More informationThe context: 6.7 billion people 1 planet. Is there a future?
Global Warming: The Scientific Basis for Anthropogenic Climate Change The context: 6.7 billion people 1 planet. Is there a future? The global average net effect of human activities since 1750 has been
More informationOverview of Global Warming, Ozone Depletion, and Air Quality
Overview of Global Warming, Ozone Depletion, and Air Quality AOSC 433/633 & CHEM 433/633 Ross Salawitch Class Web Site: http://www.atmos.umd.edu/~rjs/class/spr2013 Notes: Ross, Allison & Tim co-teach this
More informationClimate Change Science Tutorial #1: Overview of Our Understanding of the Climate System and Observed Climate Impacts
Climate Change Science Tutorial #1: Overview of Our Understanding of the Climate System and Observed Climate Impacts September 2013 ACS Climate Science Project, OMSI Others work, collected by Prof. Julie
More informationHow Climate Change Affects the Physiology of Trees
How Climate Change Affects the Physiology of Trees Jim Downer University of California Cooperative Extension ajdowner@ucdavis.edu http://ceventura.ucdavis.edu Things to consider Climate change: is it real?
More informationReport to the 10th Session of SBSTA on the Status of the IPCC Robert T. Watson, IPCC Chairman May 31, 1999
Report to the 10th Session of SBSTA on the Status of the IPCC Robert T. Watson, IPCC Chairman May 31, 1999 Distinguished delegates, it is a real pleasure and honor for me to be invited to address you today.
More informationName: Class: Date: 6. Most air pollution is produced by a. thermal inversions. c. ozone layer depletion. b. fuel burning. d. volcanic eruptions.
Name: Class: Date: Air Test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Which of the following is often used to remove poisonous gases from industrial
More informationNEW SCIENTIFIC CONSENSUS ON BLACK CARBON: AND POTENTIAL COOKSTOVE MITIGATIONS
NEW SCIENTIFIC CONSENSUS ON BLACK CARBON: AND POTENTIAL COOKSTOVE MITIGATIONS James L. Plummer Founder, IAEE President, Climate Economics Institute Las Vegas, NV plummer@ Climateeconomicsinstitute.org
More informationThe Globalization of Air Pollution:
The Globalization of Air Pollution: Implications for Air Quality, Climate and Health Regional and Global Perspectives of Air Pollution Urban Environments Interactions involve Local to Global Scales WMO
More informationThe Earth s Atmosphere-I. GEOL 1350: Introduction To Meteorology
The Earth s Atmosphere-I GEOL 1350: Introduction To Meteorology 1 Overview What is the composition of Atmosphere? How did the atmosphere arrive at its current state? 2 Earth s Atmosphere Earth s atmosphere
More informationclimate change Contents CO 2 (ppm)
climate change CO 2 (ppm) 2007 Joachim Curtius Institut für Physik der Atmosphäre Universität Mainz Contents 1. Summary 2. Background 3. Climate change: observations 4. CO 2 : ocean acidification 5. OtherGreenhouse
More informationTROPICS: insolation high year round, high sun angle and ~ constant duration
GE 101, February 6, 14 Finish insolation variation Global environmental issues associated with insolation TRPICS: insolation high year round, high sun angle and ~ constant duration MID-LATITUDES: insolation
More informationConcentrations of several of these greenhouse gases (CO 2, CH 4, N 2 O and CFCs) have increased dramatically in the last hundred years due to human
Global Warming 1.1 The facts: With no atmosphere surrounding the earth the surface temperature would be 17 o C. However, due to the greenhouse gases in the atmosphere that absorb infrared radiation emitted
More informationThe Greenhouse Effect. Greenhouse Gases. Greenhouse Gases. Greenhouse Gases
Global Warming Helen Cox, PhD Geography Department California State University, Northridge The Greenhouse Effect Science of global warming Greenhouse gases Other contributors Observed changes Temperature
More informationTODAY: TOPIC #6 WRAP UP!! Atmospheric Structure & Composition
TODAY: TOPIC #6 WRAP UP!! Atmospheric Structure & Composition There s one more thing to correct in our the depiction of incoming Solar....... the atmosphere is NOT totally TRANSPARENT to INCOMING Solar
More informationGlobal Climate Change
Global Climate Change Greenhouse Gases and Earth s Energy Balance 400 380 CO 2 in air 360 340 320 1960 1970 1980 1990 2000 2010 Year Global Climate Change 1 / 30 Outline of Topics 1 The Natural Earth System
More informationScenarios, Emissions Uncertainty, Climate Change, and Air Quality
Scenarios, Emissions Uncertainty, Climate Change, and Air Quality Steven J. Smith Joint Global Change Research Institute College Park, MD Mid-Atlantic Regional Air Management Association SIP Coordination
More informationK39: The Key Evidence That Current Global Warming is Human-Caused
K39: The Key Evidence That Current Global Warming is Human-Caused Here are 13 lines of Evidence GW = AGW (Global Warming = Anthropogenic Global Warming) Evidence #1: A Warming Troposphere with a Cooling
More informationGlobal Ocean and Atmosphere Temperature Trends Compared
Warmer Oceans result in coral bleaching and the death of coral reefs support more powerful hurricanes 32 Global Ocean and Atmosphere Temperature Trends Compared 33 Warmer Oceans and Coral Bleaching 1997-1998
More informationGLOBAL WARMING SCIENCE: PREDICTIONS, SURPRISES AND UNCERTAINTIES
Predictability in Science: Accuracy and Limitations Pontifical Academy of Sciences, Acta 19, Vatican City 2008 www.pas.va/content/dam/accademia/pdf/acta19/acta19-ramanathan.pdf GLOBAL WARMING SCIENCE:
More informationUsing An Aethalometer to Determine Optical Absorption Features from Different Black Carbon Sources
Using An Aethalometer to Determine Optical Absorption Features from Different Black Carbon Sources By: Shallena Menefield New Jersey City University Jersey City, New Jersey Background NASA/ MODIS are credited
More informationRemote Sensing (C) Team Name: Student Name(s):
Team Name: Student Name(s): Remote Sensing (C) Nebraska Science Olympiad Regional Competition Henry Doorly Zoo Saturday, February 27 th 2010 96 points total Please answer all questions with complete sentences
More informationBasics of greenhouse gases and climate change
Basics of greenhouse gases and climate change Facts and theories We need to distinguish between what we know (facts), and what we think will happen (theories). In the subject of greenhouse gases and global
More informationScientific updates on current emissions and sinks of greenhouse gases and implications for future emissions pathways
Scientific updates on current emissions and sinks of greenhouse gases and implications for future emissions pathways Dr Richard A. Houghton, Woods Hole Research Center with contributions from the Global
More informationTopic: Effects of the Atmosphere on Insolation
Topic: Effects of the Atmosphere on Insolation Sun Earth s Atmosphere 100 Units 34% reflected by atmosphere and surface 19% absorbed by the atmosphere 47% absorbed at surface Peconic Herb Farm Greenhouse
More informationGlobal Climate Change
Global Climate Change MODULE 11: GLOBAL CLIMATE CHANGE UNIT 1: BIODIVERSITY Objectives Define terms. Understand global climate change. Describe the basic predictions of the global climate models. Understand
More informationAcid deposition accumulation of potential acid-forming particles on a surface acids can result from natural causes
1 Air Quality Issues: Part 2 - Acid Deposition, Greenhouse Gases EVPP 111 Lecture Dr. Largen 2 Air Quality Issues Air Pollution Indoor Air Pollution Acid Deposition Greenhouse Gases & Global Warming 3
More informationLecture 22: Atmospheric Chemistry and Climate
Lecture 22: Atmospheric Chemistry and Climate Required Reading: FP Chapter 14 (only sections that I cover) Suggested Introductory Reading: Jacob Chapter 7 Atmospheric Chemistry CHEM-5151 / ATOC-5151 Spring
More information1.INTRODUCTION INTRODUCTION:-
1.INTRODUCTION INTRODUCTION:- From The Stone Age to the modern era man has come a long way. In his pursuit of comforts of life he ignored the threat of pollution and environmental degradation caused by
More informationDirected Reading. Section: Global Change. than in the rest of the United States. b. In the United States and Canada, many lakes are dying as their ph
Section: Global Change In the space provided, write the letter of the term or phrase that best completes each statement or best answers each question. 1. Scientists have discovered that acid rain is caused
More informationCLIMATE CHANGE AND ACID RAIN. Mr. Banks 7 th Grade Science
CLIMATE CHANGE AND ACID RAIN Mr. Banks 7 th Grade Science COMPOSITION OF AIR? COMPOSITION OF AIR? 78% Nitrogen 21% Oxygen 0.93% Argon and other noble gases 0.04% carbon dioxide Variable amounts of water
More information