E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Solomon et al., 2007 Chapter.

Slides:



Advertisements
Similar presentations
Short Background on Climate Change and Greenhouse Gases Dr Ruth Nussbaum ProForest Presentation to the RSPO GHG WG2 meeting in Feb 2010.
Advertisements

Michael B. McElroy ACS August 23rd, 2010.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Radiative Forcing (from IPCC WG-I, Chapter 2) Changes in Radiative Forcing Primary Source: IPCC WG-I Chapter.
Greenhouse Gases and Energy Budget LP 3 1. What are the greenhouse gases? Where do they come from? How do they work? 2.
Climate Change. Climate change: Changes in many climatic factors. Global warming: The rise in global temperatures.
4.4 Climate Change.
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
Climate change slides.
Rising Temperatures. Various Temperature Reconstructions from
1 Lecture 15: Projections of Future Climate Change Global Mean Temperature.
The Greenhouse Effect Presenters: Jaime Pinto & Nathalie Mokuba
The Science of Climate Change Why We Believe It and What Might Happen Dave Stainforth, University of Exeter Tyndall Centre for Climate Change Research.
R21 Global Warming & Greenhouse Effect Prior Knowledge: What do you know about Greenhouse Effect and Global Warming?
Chapter 2 frontispiece. The crescent moon as seen through Earth’s thin upper atmosphere E.A. Mathez, 2009, Climate Change: The Science of Global Warming.
Weather Condition of the atmosphere at any particular time and place Air temperature, air pressure, humidity, clouds, precipitation, visibility, wind Climate.
FROM AIR POLLUTION TO GLOBAL CHANGE AND BACK: Towards an integrated international policy for air pollution and climate change Daniel J. Jacob Harvard University.
National Aeronautics and Space Administration The Energy Budget and the Greenhouse Effect Dr. Lin H. Chambers, NASA Langley Research Center.
The latest science on the climate change challenge David Karoly, Univ of Melbourne TC Larry, 2006 From Bureau of Meteorology.
Climate--The average weather over years and longer… Chapter 1 frontispiece. Satellite view looking east from Patagonia over southern Argentina and the.
Global Warming Cause for Concern. Cause for Concern? What is the effect of increased levels of carbon dioxide in the Earth’s atmosphere? Nobody knows.
EEA/JRC/WHO report on impacts of climate change in Europe 3 rd Advisory Group meeting Copenhagen, 23 April 2008 Introductory chapters André Jol,
Understanding the Greenhouse Effect The Impact of the Greenhouse gases on the Earth.
Greenhouse Effect.  The greenhouse effect is the warming of the surface and lower atmosphere of Earth that occurs when carbon dioxide, water vapor, and.
Greenhouse Gases and Energy Budget LP 3 1. What are greenhouse gases? Where do they come from? How do they work? 2.
Southwest Regional Climate Hub Developed by the Asombro Institute for Science Education (
Anthropogenic Climate Change. Global Temperature is Increasing.
The Greenhouse Effect and Global Warming. What is the greenhouse effect? ms/greenhouse/
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
Global Changes in the Atmosphere
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Chapter 5 frontispiece. A dust plume from an intense dust storm over the Sahara E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our.
Mr. Fleming. The trapping of heat from the sun by gases in the Earth’s atmosphere. The major gas contributing to this process is Carbon dioxide gas.
The trapping of heat from the sun by gases in the Earth’s atmosphere. The major gas contributing to this process is Carbon dioxide gas. Greenhouse effect.
The Greenhouse Effect. Some atmospheric basics The greenhouse effect Radiant energy that is absorbed heats Earth and eventually is reradiated skyward.
Chapter 7 frontispiece. The Sahel of Africa E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University.
What is Climate Change?. Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words,
Chapter 6 Future climate changes Climate system dynamics and modelling Hugues Goosse.
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
Global Warming Nicholas DeJarnette. What is global warming? Global warming is the overall rise in the temperature on the Earth’s surface.
LO: To be able to interpret graphs to explain if the climate is changing To be able to construct a diagram to show the greenhouse effect To explain the.
Global Warming Vs Climate Change
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
Atmosphere. Earth’s Radiation Budget Earth maintains an energy balance and a temperature balance by radiating as much energy into space as it absorbs.
Warmup What are three natural ways in which climate changes? What timescale do these processes generally occur?
The Greenhouse Effect. Natural heating of earth’s surface caused by greenhouse gases –CO 2 (Carbon Dioxide) –CH 3 (Methane) –N 2 O (Nitrous Oxide) –H.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Aspire: Challenge: Examine and use evidence to justify whether the causes of climate change are caused by humans or natural factors. Explain how the Earths.
What is global warming? Discuss with your table what global warming is. You have 1 MINUTE!!!
CHAPTER 13 – ATMOSPHERE AND CLIMATE CHANGE Section 3a – Climate Change.
Greenhouse Gases: Effects of Warming Emerson Middle School.
1. Global Climate Change refers to…?:
The Greenhouse Effect 8.6 The greenhouse effect is a natural process whereby gases and clouds absorb infrared radiation emitted by Earth’s surface and.
The Greenhouse Effect.
Greenhouse effect The trapping of heat from the sun by gases in the Earth’s atmosphere. The major gas contributing to this process is Carbon dioxide gas.
Global warming By: J.W..
Global Climate Change Video
Climate Dynamics 11:670:461 Alan Robock
Greenhouse Effect Presented By: Janet Fang Sam Atwood EESC W4400.
AVERAGE JANUARY TEMPERATURE (°F)
Global Warming Effects of increase CO2
Satellite mosaic image of Shanghai, at the mouth of the Yangtze River and one of China’s megacities threatened by rising sea level J. Stevens and J. Allen,
Points for discussion Have human activities changed the composition of Earth’s atmosphere? Has Earth’s temperature changed in the past 150 years? In the.
Climate Change.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Greenhouse Effect.
Table 1-1, p.3.
Threats to Biodiversity Climate Change
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Greenhouse Effect.
The Greenhouse Effect and Global Warming
Presentation transcript:

E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Solomon et al., 2007 Chapter 9 Frontispiece. A multiclimate model average projection of global surface temperature changes in the decade compared with the years

Figure 9.1. Modeling global mean surface temperature E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Hegerl et al.,

E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Hegerl et al., 2007 Figure 9.2. Spatial distribution of observed warming compared with the distribution obtained from model simulations, and

Figure 9.3. Projected changes in mean global surface temperature under three emissions scenarios E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: IPCC,

Figure 9.4. Projected changes in temperature, precipitation, and sea-level air pressure for winter (December-February) and summer (June-August), E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: Meehl et al.,

Table 9.1. Changes in the growth of carbon dioxide (CO 2 ) emissions required by 2050 to bring about specific warming targets E.A. Mathez, 2009, Climate Change: The Science of Global Warming and Our Energy Future, Columbia University Press. Source: IPCC, to to to to to to +140 a CO 2 -eq is the concentration of CO 2 that would have the same radiative forcing as the forcing due to all the greenhouse gases (CO 2, methane, nitrogen oxide, ozone, halocarbons). b The equilibrium global mean temperature = temperature at the same time the climate finally stops changing (i.e. after all the committed warming has occurred) above the pre-industrial temperature. Additional Radiative Forcing (W/m 2 ) Atmospheric CO 2 Contents (ppm) CO 2 -eq Contents (ppm) a Target Temperature Increase b (°C) Peak Year for Emissions Change in Emissions By 2050 (% of 2000 Emissions) 103