Lecture #7 Integrated Assessment of Climate and Carbon Cycle Atul K. Jain Department of Atmospheric Sciences University of Illinois, Urbana, IL email:

Slides:



Advertisements
Similar presentations
On-line resource materials for policy making Ex-Ante Carbon-balance Tool Food and Agriculture Organization of the United Nations, FAO Learning how using.
Advertisements

1 Assessment of contributions to climate change Dennis Tirpak UNFCCC secretariat.
1 On-line resource materials for policy making Ex-Ante Carbon-balance Tool Food and Agriculture Organization of the United Nations, FAO Learning how using.
CMIP5: Overview of the Coupled Model Intercomparison Project Phase 5
Factors to be considered in choosing metrics Shengmin Yu Energy Research Institute of NDRC, China Bonn, April 2012 Workshop on common metrics to calculate.
Challenges and Needs in Research Views of Japan -emerging challenges and policy needs- Hiroki Kondo Advisor to the Ministry of Education, Culture, Sports,
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
Carbon Dioxide Simulator Data from: 1.
What is the point of this session? To use the UK’s experience to give ideas about creating and using climate change scenarios in other countries and situations.
Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009 Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009.
Global Warming and Climate Sensitivity Professor Dennis L. Hartmann Department of Atmospheric Sciences University of Washington Seattle, Washington.
Chalmers University of Technology Metrics and stabilization of the global average surface temperature Daniel J.A. Johansson Division of Physical Resource.
Discussion Space Research Centre. Urbanization and Industrialization: in 2008, more than half of humans live in cities UN Population Report 2007.
Carbon Sequestration Akilah Martin Fall Outline Pre-Assessment  Student learning goals  Carbon Sequestration Background  Century Model Overview.
Climate Change: An Overview of the Science Anthony J. Broccoli Director, Center for Environmental Prediction Department of Environmental Sciences Rutgers.
MET 112 Global Climate Change - Lecture 11 Future Predictions Craig Clements San Jose State University.
Anthropocene Introduction to Meteorology, spring 2011 Observations –Trace gases –Temperature, land and ocean –Precipitation –Sea level Attribution Models.
Your Name Your Title Your Organization (Line #1) Your Organization (Line #2) Global warming.: Matthieu BERCHER, Master M.I.G.S., University of Burgundy,
1 Global Change: Greenhouse Gases Environmental Sustainability Educational Resources prepared by Gregory A. Keoleian Associate Research Scientist, School.
The Anthropogenic Ocean Carbon Sink Alan Cohn March 29, 2006
Radiation’s Role in Anthropogenic Climate Change AOS 340.
1 Lecture 15: Projections of Future Climate Change Global Mean Temperature.
Climate Change: Carbon footprints and cycles. What is climate change? What do you think climate change is? What do we actually mean when we talk about.
How is the average temperature of Earth determined? Jot down a few ideas Sketch a map of the room. Show the locations of each water container. When directed,
US CLIVAR Themes. Guided by a set of questions that will be addressed/assessed as a concluding theme action by US CLIVAR Concern a broad topical area.
Using Earth System Models to provide policy-relevant information (Couples therapy for the uneasy marriage between science and policy)‏ Gavin Schmidt NASA.
Climate Change Curriculum: UPM Experiences

Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
A current world debate. Colorado Prepared Graduate Competencies: Evaluate evidence that the Earth is a complex system of interactions between the geosphere,
Energy & Its Impact on Global Society Jerome K. Williams, Ph.D. Saint Leo University Dept. Mathematics & Sciences.
Report on March Crystal City Workshop to Identify Grand Challenges in Climate Change Science By its cochair- Robert Dickinson For the 5 Sept
Results from UIUC Simple Climate Model Evaluation of the Relative Contributions of the Regional Emissions by Annex I and Non-Annex I to the Historical.
PROSPERIDAD J. ABONETE JULY 3, 2003 Understanding Climate Change.
24 Global Ecology. Figure 24.2 A Record of Coral Reef Decline.
June 2011 The UNEP Java Climate Model Cindy Shellito University of Northern Colorado.
Metrics for quantification of influence on climate Ayite-Lo Ajovan, Paul Newman, John Pyle, A.R. Ravishankara Co-Chairs, Science Assessment Panel July.
Global Warming - 1 An Assessment The balance of the evidence... PowerPoint 97 PowerPoint 97 To download: Shift LeftClick Please respect copyright on this.
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
INTERGOVERNMENTAL PANEL ON CLIMATE CHANGE (IPCC) Working Group I Working Group I Contribution to the IPCC Fourth Assessment Report Climate Change 2007:
IPCC WG1 AR5: Key Findings Relevant to Future Air Quality Fiona M. O’Connor, Atmospheric Composition & Climate Team, Met Office Hadley Centre.
© Crown copyright Met Office AR5 Proposed runs for CMIP5 John Mitchell, after Karl Taylor, Ron Stouffer and others ENES, arch 2009.
PROJECT TO INTERCOMPARE REGIONAL CLIMATE SIMULATIONS Carbon Dioxide and Climate Change Eugene S. Takle Agronomy Department Geological and Atmospheric Science.
Greenhouse Effect and Greenhouse Gases. GREENHOUSE FFECTFFECT.
Anthropocene physical basis of climate spring 2011 Introduction and UNEP reports Observations –Emissions and other natural forcingsEmissions and other.
Newton Paciornik BRAZIL Policy Goals and Common Metrics Implications Bonn, 04 April 2012 Workshop on common metrics to calculate the CO 2 equivalence of.
The evolution of climate modeling Kevin Hennessy on behalf of CSIRO & the Bureau of Meteorology Tuesday 30 th September 2003 Canberra Short course & Climate.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 1: An Introduction Don Wuebbles Department of Atmospheric Sciences University of Illinois,
Climate Change – Defra’s Strategy & Priorities Dr Steven Hill Department for Environment Food and Rural Affairs 22 nd May 2007 FLOODING DESTRUCTION AT.
Modelling the climate system and climate change PRECIS Workshop Tanzania Meteorological Agency, 29 th June – 3 rd July 2015.
Integrated Assessment and IPCC: Links between climate change and sub-global environmental issues presentation at Task Force Integrated Assessment Modelling,
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 14: Methane and CO Don Wuebbles Department of Atmospheric Sciences University of Illinois,
Intergovernmental Panel on Climate Change (IPCC) The IPCC is the leading international body for the assessment of climate change. It was established by.
© Crown copyright Met Office Uncertainties in the Development of Climate Scenarios Climate Data Analysis for Crop Modelling workshop Kasetsart University,
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 12 Future Predictions Eugene Cordero San Jose State University Outline  Scenarios.
CLIMATE CHANGE PROJECTIONS: SOURCES AND MAGNITUDES OF UNCERTAINTY Tom Wigley, National Center for Atmospheric Research, Boulder, CO 80307, USA
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 25: Climate, Energy and Carbon Sequestration Don Wuebbles Department of Atmospheric Sciences.
Radiative Forcing of Climate Change: Expanding the Concept and Addressing Uncertainties Report from the NRC Committee on Radiative Forcing of Climate commissioned.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Carbon Sequestration Akilah Martin Fall 2005.
Pre-anthropogenic C cycle and recent perturbations
MAGICC/SCENGEN Model for Assessment of Greenhouse-gas Induced Climate Change/A Regional Climate SCENario GENerator.
IPCC Climate Change 2013: The Physical Science Basis
Chapter 19 Global Change.
USAEE Conference 2016, October 26, Tulsa, Oklahoma, USA
Anthropocene physical basis of climate spring 2011
National Center for Atmospheric Research
Climate Change – Examining the Evidence
Presentation transcript:

Lecture #7 Integrated Assessment of Climate and Carbon Cycle Atul K. Jain Department of Atmospheric Sciences University of Illinois, Urbana, IL ATMOS 397G Biogeochemical Cycles and Global Change

How Much is a % Contribution of CO 2 in the Atmosphere  25%  10%  5%  1% or less

Why Model The Carbon Cycle Increasing atmospheric CO2 content may significantly alter Earth's climate and biosphere in the next century To predict climate and its impacts, we need to be able to predict future CO2 concentrations

CO 2 is the Single Most Important GHG Observed Atmospheric CO2 Concentration ( )

Human Activities Perturb Natural Carbon Cycle Land Use Fossil Fuel

Carbon Cycle Modeling  The ability to predict the response of the carbon cycle to anthropogenic emissions relies on the:  Understanding of Carbon Cycle Mechanisms  Ocean transport and chemistry, and, air/sea exchange  plant physiology and soil processes  CO 2 & Nitrogen Fertilization  Forest regrowth  Response to climate change  Measured behavior of the past carbon cycle  CO2 Fossil Fuel and Cement emissions  Observed CO 2 concentration  Observed distribution of carbon isotopes ( 12 C, 13 C, 14 C)

Industrial Society & the Global Carbon Cycle Units: Gt C and Gt C y -1 Atmosphere Fossil Deposits Plants Soil Surface Ocean ,000 About 16, …are leading to a build up of CO 2 in the atmosphere. Fossil emissions... …and land clearing in the tropics... IPCC (2001) Intermediate & Deep Ocean 1,

  Jain et al. (1996) 13 C Evidence in the Atmosphere and Ocean Points to Link Between Human-Related Emissions and CO 2 Rise Model Validation

Global CO 2 Budget (GtC/yr) Based on Atmospheric CO 2 and O 2 Data The global CO 2 budget is usually defined as the mass balance among sources and sinks of CO 2 produced by human activities. Balancing the global CO 2 budget requires a large unidentified (“missing”) carbon sink on land. (The transfers shown (in metric tones of carbon per year) represent the CO 2 budget for the 1980’s and 1990’s as estimated by the IPCC (1996 and 2001). 1.6 ± ± ± ± 0.53 ± ??? 1990s 1980s

Natural Transfers Fluctuate over Short Time Scale Rate of increase of CO 2 Assessment of the Global CO 2 Budget Requires Long Term Measurements and Models

ISAM Estimated CO 2 Concentrations for IS92a Scenario

GREENHOUSE GAS EMISSIONS SCENARIOS Purposes:  to develop an understanding of how human-related emissions will affect future climate  to enable us to look ahead & evaluate potential impacts for the range of possible future changes in climate  to be able to accurately compare present GHG emission reduction costs with future damages

Future Projections Future Projections Major Uncertainties Socioeconomic (Future Emissions SRES Scenarios) Carbon Cycle (Resulting CO 2 Concentration) and Climate Sensitivity (ºC for 2  CO 2 ) Based on ISAM

Impact of Stabilizing Emissions versus Stabilization Concentrations of CO 2

The Challenge of Stabilization of Atmospheric Concentrations of Carbon Dioxide IPCC (2001, Based on ISAM) Emissions of CO 2 due to fossil fuel burning will be the dominant influence on atmospheric CO 2 in the 21st century Emissions of CO 2 due to fossil fuel burning will be the dominant influence on atmospheric CO 2 in the 21st century Stabilization of CO 2 at twice the pre-industrial level will require emissions to drop to below 1990 levels in less than 50 years. Stabilization of CO 2 at twice the pre-industrial level will require emissions to drop to below 1990 levels in less than 50 years. Emissions will need to continue to decrease steadily thereafter to a very small fraction of current emissions. Emissions will need to continue to decrease steadily thereafter to a very small fraction of current emissions.

Cumulative Carbon Emission Ranges for WRE Scenarios (2100) WRE Range of Cumulative Emission

A Grand Challenge: Study Feedbacks Throughout The Earth System In the science and policy world … EMISSIONS Socio-economic + energy analyses and modeling CONCENTRATIONS Carbon Cycle & Chemical transport models CLIMATE CHANGE IMPACTS RADIATIVE FORCING Radiative transfer models A-O-CIRCULATION A-O Models

Integrated Assessment

Tying it all together: The Concept of Integrated Assessment Modeling (IAM) l Purpose:  to interface science with policy  to provide information of use to decision-makers, not just for the sake of increasing knowledge for knowledge’s sake alone  to provide insights that cannot be easily derived from individual component models

Modeling the Earth-Climate System: Components

Integrated Assessment Modeling “Integrated” refers to:  the completeness of causal links cycle coverage  the inclusion of feedback loops within and between cause-effect chains  the bringing together of information & analysis from disparate disciplines “Assessment” refers to:  the focus of the models on evaluation and assessment of human & natural contributions and responses to climate change

What would the ideal IAM look like? It would:  model the complete causal chain, including all feedbacks  have an interface that could be used interactively by a reasonably educated policy-maker on their own desktop PC  have results that don’t differ significantly from a hypothetical IAM made of the most comprehensive models available

The Integrated Science Assessment Model (ISAM) ISAM is:  a deterministic projection, policy evaluation model  capable of evaluating climatic impacts of one policy decision at a time  a process-oriented model  has a modular structure with sub-models being simplified versions of models from different scientific disciplines, with standardized assumptions

Integrated Science Assessment Model (ISAM) Earth System Model of Intermediate Complexity EMISSIONS PNNL MiniCam Model GHG emissions from industrial & energy-related sources CHEMICAL TRANSPORT 2D Atmospheric Chemical Transport Box Model Concentrations of GHG,aerosols and other radiatively active species BIOSPHERE Agricultural Land Use Model CO2 fluxes from land use change CARBON CYCLE 2D Coupled Atmosphere- Ocean-Biosphere Model Carbon dioxide concentrations CLIMATE MODEL 2D Radiative Transfer Model 2D Atmosphere-Ocean-Land Moisture & Energy Balance Model Changes in global temperature, precipitation and sea level IMPACT ASSESSMENT STUDIES

Integrated Science Assessment Model (ISAM) as Tool for Scientific and Policy Analysis UUse all key Climate System Components and Feedbacks at an appropriate level of detail; AAccount sub-grid climate processes by using empirical relationships to approximate net effects; AApproximate the effects of various physical and chemical processes based on AOGCM and CTM DDesign to Upgrade as knowledge improves; EEvaluate Chemical and Climate Feedback Effects on Policy Developments; TTreat Uncertainty as an Essential Feature; GGlobal in scope, but resolve regional distribution.

GOAL - ISAM The development of an ideal tool based on solid science to increase our understanding of earth system feedbacks and to address multi-dimensional science and policy issues related to climate change.

Global-Annual Mean Version of Integrated Science Assessment Model (ISAM)

ISAM WWW INTERFACE Purpose:  To make a state-of-the-art integrated assessment model available to the general public in a user-friendly format

ISAM Interface - Objectives To give students/Educators/Policy Makers a tool for:  understanding the science of global change using ISAM students see how physical processes and parameters in the climate system determine its behavior  understanding the long-term consequences of near-term policy choices model outputs show long residence times of greenhouse gases in the atmosphere  understanding how policy makers assess the implications of their decisions students use a model identical to that used by policy makers in forming greenhouse gas emissions policies

WWW INTERFACE OF ISAM ( This Interface Enables the User to  Run the ISAM on the Web Using an Intuitive Menu System  Alter the Various Physical Formulations of ISAM  Construct Scenarios of Greenhouse Gas and aerosol emissions  Assess their Impact on the Global Climate and on Sea Level Results are Presented as Graphs and Tables

Users of Our Web Site Students of climate, and climate change, investigating the past and future effects of anthropogenic climate forcings. Students of public policy studying the implications of proposed greenhouse-gas mitigation strategies. Educators preparing course material on the science of global climate change and the implications of greenhouse-gas mitigation strategies. Policy makers, in both government and the private sector, seeking projections of how their decisions will affect future greenhouse-gas concentrations and climate change.

Model Inputs Step 1: Model Formulation for the Steady State:  Use default model settings or alter parameter values Question to answer: What are the implications of different values for climate sensitivity? Step 2: Model Calculations of the Greenhouse Effect from Pre-Industrial Times into the Future  Run the model based on the Historical Observed Data, Question to answer: How well does the model reproduce past climate change? How does this depend on model parameters?  Prescribe the Future Emission Scenario for Dates after 1990 a) Select IPCC (Intergovernmental Panel on Climate Change) Scenarios for OR... Specify emissions of major greenhouse gases (CO2, CH4, N2O, CFCs, SO2) in key years. (b) Select end year of calculation (> 1995)

Model Output Results Available as Graphs and Tables include:  Temperature Change and Rate of Temperature Change  Sea Level Change and Rate of Sea Level Change  Historical CO 2 Emissions, Fluxes, and Atmospheric Concentrations  Future Emissions of Major Greenhouse Gases (CO 2, CH 4, CO, OH, N 2 O, CFCs, and SO 2 )  Concentrations of Major Greenhouse Gases  Total Tropospheric Chlorine and Ozone Changes  Radiative Forcings for Major Greenhouse Gases and Aerosols

THE END