Oaverview of IPCC reports Kyoto, Copenhagen, Russia’s & America’s Role, IPCC Reports etc. June 2, 2014 Return to Home Page.

Slides:



Advertisements
Similar presentations
Greenhouse Gases and Climate Change: Global Changes and Local Impacts Anthony J. Broccoli Director, Center for Environmental Prediction Department of Environmental.
Advertisements

Jeffery Spooner (Climate Branch Head) Meteorological Service, Jamaica International Day for Biological Diversity: Biodiversity and Climate Change 22 May.
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.
1 Weather and Climate Bay Area Earth Science Institute (BAESI) Climate San Jose State University, January 24, 2004
Pacific Northwest Climate Model Scenarios 2008 Climate Impacts Group & Department of Atmospheric Sciences University of Washington Eric Salathé Philip.
Intergovernmental Panel on Climate Change Presentation Based on the Fourth Assessment Report Climate Change 2007.
New climate change scenarios for the Pacific Northwest Eric Salathé Climate Impacts Group University of Washington.
May 2007 vegetation Kevin E Trenberth NCAR Kevin E Trenberth NCAR Weather and climate in the 21 st Century: What do we know? What don’t we know?
The Earth in Climate change – will humanity follow the Polar Bear and the Great Barrier Reef?
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
Brief Climate Discussion William F. Ryan Department of Meteorology The Pennsylvania State University.
The Science of Climate Change - Overview
Rising Temperatures. Various Temperature Reconstructions from
5. Future climate predictions Global average temperature and sea-level are projected to rise under all IPCC scenarios Temperature: +1.8°C (B1) to +4.0°C.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Observed Surface & Atmosphere (from IPCC WG-I, Chapter 3) Observed Changes in Surface and Atmosphere Climate.
Turn Down the Heat: State of the Climate (and Australia) February 2014 Damien Lockie.
Climate Change – 1: Background
An update on the science of climate change David Karoly School of Earth Sciences, University of Melbourne TC Larry, 2006 From Bureau of Meteorology.
Climate Variability and Change: An Overview Leigh Welling Crown of the Continent Research Learning Center Glacier National Park.
3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.
DAILY REVIEW #9 29. What happens in the Arctic Ocean that drives the thermohaline circulation? 30. Why is the thermohaline circulation important to climate?
Global Warming Inez Fung University of California, Berkeley April 2007.
Outline Further Reading: Detailed Notes Posted on Class Web Sites Natural Environments: The Atmosphere GE 101 – Spring 2007 Boston University Myneni L30:
Evidence for climate Change The Working Group I Report of the Intergovernmental Panel on Climate Change Fourth Assessment Report Nathan Bindoff and others.
Climate Lesson What factors contribute to a region’s climate?
Dave Siegel Director, Institute for Computational Earth System Science Professor, Department of Geography March 22, 2007 Global Warming & You.
© Crown copyright Met Office Extreme weather and climate change Dr Peter Stott, Met Office Hadley Centre.
Impact of Climate Change on Water Resources Water Corporation Technical Seminars 10 July 2006 Brian Ryan CSIRO Marine and Atmospheric Research.
The La Niña Influence on Central Alabama Rainfall Patterns.
Ocean Circulation: El Niño
Climate Change 101. What Is Climate? What Is the Greenhouse Effect?
(Slide Source: William J. Gutowski, Jr., Iowa State University) The Science of Climate Change - Overview Primary Source: IPCC WG-I - Summary for Policymakers.
Modern Climate Change Darryn Waugh OES Summer Course, July 2015.
Teleconnections Current Weather Current Weather Finish ENSO Finish ENSO North Atlantic and Arctic Oscillations North Atlantic and Arctic Oscillations Pacific.
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
International Environment Forum Conference Ottawa October 12 th, 2007 John M R Stone Carleton University.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Climate Models (from IPCC WG-I, Chapter 10) Projected Future Changes Primary Source: IPCC WG-I Chapter 10 - Global.
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.
In Northern Mists: Bering Climate-Present and Future James Overland, Phyllis Stabeno, Muyin Wang and Nick Bond NOAA/Pacific Marine Environmental Laboratory.
Anthropocene physical basis of climate spring 2011 Introduction and UNEP reports Observations –Emissions and other natural forcingsEmissions and other.
What is Climate Change? Dan Hodson EC110 Economics of Climate Change.
Climate Change Information Seminar Intergovernmental Panel on Climate Change Fourth Assessment Report (AR4) – the relevance to FAO’s activities Claudia.
7 th SPC HOF meeting Observed and projected changes to Pacific surface climate Janice Lough (AIMS) Jerry Meehl (NCAR) and Jim Salinger (NZ)
Consequences of Global Warming (IPCC SPM-AR4) 1)Reduced uptake of CO2 by land and ocean in warmer climate 2)Rising sea levels (0.3 to 0.6m by 2100)…. at.
Climates can change suddenly or slowly.  ICE AGE: Period in which huge sheets of ice spread out beyond the polar regions.  El NINO: A disturbance of.
Dr. Alan F. Hamlet Skagit Climate Science Consortium Climate Impacts Group Dept. of Civil and Environmental Engineering, University of Washington Climate.
El Niño–Southern Oscillation (ENSO): What is it?
Lecture 15 (Review) Ocean’s Role in Climate and Climate Change by Instructor: Dr. Charles Dong at El Camino College.
Global Impacts and Consequences of Climate Change
detection, attribution and projections
Climate Change slides for Exam Two
Global Warming Michael E. Mann, Department of Environmental Sciences
What factors contribute to a region’s climate?
Lecture 15 (Review) Ocean’s Role in Climate and Climate Change by Instructor: Dr. Charles Dong at El Camino College.
Chapter 14: Climate Change
AVERAGE JANUARY TEMPERATURE (°F)
EVSC 1300 Global Warming.
El Nino Southern Oscillation
Anthropocene physical basis of climate spring 2011
Changes in surface climate of the tropical Pacific
Temperature and CO2 Trends.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
El Niño and the Southern Oscillation (“ENSO”)
Changes in surface climate of the tropical Pacific
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Changes in surface climate of the tropical Pacific
Changes in surface climate of the tropical Pacific
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Inez Fung University of California, Berkeley April 2007
Presentation transcript:

Oaverview of IPCC reports Kyoto, Copenhagen, Russia’s & America’s Role, IPCC Reports etc. June 2, 2014 Return to Home Page

IPCC - WGI Source: Thompson et al ENSO = El Nino/ Southern Oscillation COWL= cold ocean, warm land

IPCC - WGI Source: Thompson et al., 2008.

IPCC - WGI Source: Thompson e tal., 2008.

Observed Vs. modeled temperature rise since 1860

Computer Model Comparison of Anthropogenic and Natural Forcing (red) vs. Only Natural Forcing (blue) Figure 10.31

IPCC - WGI Understanding and Attributing Climate Change Anthropogenic warming is likely discernible on all inhabited continents Observed Expected for all forcings Natural forcing only

1000 Years of CO 2 and Temperatures Figure 10.29

Fig Global temperature trends, Annual & five-year means, the 0 baseline represents the global average - which is 14ºC (52.2ºF).

INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I

Temperature trends

Temperature Anomalies Figure 10.30

10,000 Years of Greenhouse Gases Figure 10.32

Figure 10.34

What’s in the pipeline and what could come Warming will increase if GHG increase. If GHG were kept fixed at current levels, a committed 0.6°C of further warming would be expected by More warming would accompany more emission. 1.8 o C = 3.2 o F 2.8 o C = 5.0 o F 3.4 o C = 6.1 o F CO2 Eq o C = 1.0 o F

Surface Temperature Projections Figure 10.35

Changing winds, temperatures and storm tracks Anthropogenic forcing has likely contributed to circulation changes (storm tracks, winds and temperature patterns) Warmer, wetter winters in Norway; drier in Spain (and North Africa) Warmer, wetter winters in Norway; drier in Spain (and North Africa) Source: IPCC 2007, Working Group 1, AR4 (Assessment Report 4).

A1B is a typical “business as usual” ( ) scenario: Global mean warming 2.8 o C; Much of land area warms by ~3.5 o C Arctic warms by ~7 o C; would be less for less emission

Projections of Future Changes in Climate New in AR4: Drying in much of the subtropics, more rain in higher latitudes, continuing the broad pattern of rainfall changes already observed.

Emissions & Stabilization Wedges