magicc/scengen hands on tutorial
DESCRIPTION
MAGICC/SCENGEN Hands On Tutorial. By Joel B. Smith Stratus Consulting Inc. [email protected] NCAR Summer 2006 Colloquium on Climate and Health July 18, 2006. Outline. Brief Introduction on Climate Change Scenarios - PowerPoint PPT PresentationTRANSCRIPT
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MAGICC/SCENGEN Hands On Tutorial
By
Joel B. Smith
Stratus Consulting Inc.
NCAR Summer 2006 Colloquium on Climate and Health
July 18, 2006
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Outline
• Brief Introduction on Climate Change Scenarios
• Then, we’ll spend most of the time on the tutorial on MAGICC/SCENGEN
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Why Use Climate Change Scenarios?
• We are unsure exactly how regional climate will change
• Scenarios are plausible combinations of variables consistent with what we know about human-induced climate change
• One can think of them as the prediction of a model, contingent upon the greenhouse gas emissions scenario
• Since estimates of regional change by models differ substantially, an individual model estimate should be treated more as a scenario
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What Are Reasonable Scenarios?
• Scenarios should be:– Consistent with our understanding of the anthropogenic
effects on climate
– Internally consistent • e.g., clouds, temperature, precipitation
• Scenarios are a communication tool about what is known and not known about climate change– Should reflect plausible range for key variables
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Scenarios for Impacts Analysis
• Need to be at a scale necessary for analysis
• Spatial – e.g., to watershed or farm level
• Temporal – Monthly– Daily– Sub-daily
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Regional Climate Change Scenarios
• Present range of possible regional changes in climate
• Two roles– Use ranges of climate changes to help
understand sensitivity of affected systems– Use ranges to communicate what is known and
not known about regional climate change• Temperature rise and range of precipitation changes
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Tools for Assessing Regional Model Output
• We’ll learn how to use a tool that enables us to examine output from a number of climate models
• Can see degree to which models agree and disagree about regional changes
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Sources of Uncertainty on Regional Climate Change
• GHG Emissions
• Greenhouse Gas Concentrations
• Climate Sensitivity, e.g., 2xCO2
• Regional pattern of climate change– Distribution of changes in temperature and precipitation
• Climate Variability
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GHG Emissions and Concentrations Projections
Source: Houghton et al., 2001.
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Projections of Global Mean Temperature Change
Source: Houghton et al., 2001.
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Normalized Annual-Mean Temperature Changes in CMIP2 Greenhouse Warming
Experiments
0.2
0.4
0.6
0.8
1
1.2
1.4
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MAGICC/SCENGEN
• User can:– Select GHG emission scenarios e.g., from IPCC
SRES– Can select CO2 concentration– Select climate sensitivity– Select GCMs to examine
• Regional pattern is hard wired in
– Can examine change in seasonal variability• Not interannual or daily
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MAGICC/SCENGEN• MAGICC is a simple model
of global T and SLR• Used in IPCC TAR• SCENGEN uses pattern
scaling for 17 GCMs• Yield
– Model by model changes– Mean change– Intermodel SD– Interannual variability
changes– Current and future climate on
5 x 5°grid
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Using MAGICC/SCENGEN
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MAGICC: Selecting Scenarios
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SO2 Scenarios
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MAGICC: Selecting Scenarios (continued)
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MAGICC: Selecting Forcings
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MAGICC: Displaying Results
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MAGICC: Displaying Results (continued)
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SCENGEN
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Normalizing GCM Output
• Expresses regional change relative to an increase of 1°C in mean global temperature– This is a way to avoid high sensitivity models
dominating results– It allows us to compare GCM output based on relative
regional change
• Normalized temperature change = ΔTRGCM/ΔTGMTGCM
• Normalized precipitation change = ΔPRGCM/ΔTGMTGCM
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Pattern Scaling• Is a technique for estimating change in
regional climate using normalized patterns of change and changes in GMT
• Pattern scaled temperature change: – ΔTRΔGMT = (ΔTRGCM/ΔTGMTGCM) x ΔGMT
• Pattern scaled precipitation– ΔPRΔGMT = (ΔPRGCM/ΔTGMTGCM) x ΔGMT
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Running SCENGEN (continued)
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SCENGEN: Analysis
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SCENGEN: Model Selection
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SCENGEN: Area of Analysis
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SCENGEN: Select Variable
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SCENGEN: Scenario
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SCENGEN: Global Results
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SCENGEN: Map Results
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SCENGEN: Quantitative ResultsINTER-MOD S.D. : AREA AVERAGE = 5.186 % (FOR NORMALIZED GHG DATA) INTER-MOD SNR : AREA AVERAGE = -.067 (FOR NORMALIZED GHG DATA) PROB OF INCREASE : AREA AVERAGE = .473 (FOR NORMALIZED GHG DATA) GHG ONLY : AREA AVERAGE = -.411 % (FOR SCALED DATA) AEROSOL ONLY : AREA AVERAGE = -.277 % (FOR SCALED DATA) GHG AND AEROSOL : AREA AVERAGE = -.687 % (FOR SCALED DATA) *** SCALED AREA AVERAGE RESULTS FOR INDIVIDUAL MODELS *** (AEROSOLS INCLUDED) MODEL = BMRCD2 : AREA AVE = 2.404 (%) MODEL = CCC1D2 : AREA AVE = -5.384 (%) MODEL = CCSRD2 : AREA AVE = 6.250 (%) MODEL = CERFD2 : AREA AVE = -2.094 (%) MODEL = CSI2D2 : AREA AVE = 6.058 (%) MODEL = CSM_D2 : AREA AVE = 1.245 (%) MODEL = ECH3D2 : AREA AVE = .151 (%) MODEL = ECH4D2 : AREA AVE = -1.133 (%) MODEL = GFDLD2 : AREA AVE = 1.298 (%) MODEL = GISSD2 : AREA AVE = -3.874 (%) MODEL = HAD2D2 : AREA AVE = -5.442 (%) MODEL = HAD3D2 : AREA AVE = -.459 (%) MODEL = IAP_D2 : AREA AVE = -.088 (%) MODEL = LMD_D2 : AREA AVE = -6.548 (%) MODEL = MRI_D2 : AREA AVE = .065 (%) MODEL = PCM_D2 : AREA AVE = -3.451 (%) MODEL = MODBAR : AREA AVE = -.687 (%)
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SCENGEN: Global Analysis
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SCENGEN: Error Analysis
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SCENGEN Error Analysis (continued)
UNWEIGHTED STATISTICS MODEL CORREL RMSE MEAN DIFF NUM PTS mm/day mm/day BMRCTR .632 1.312 1.026 20 CCC1TR .572 1.160 -.207 20 CCSRTR .587 .989 .322 20 CERFTR .634 1.421 -1.167 20 CSI2TR .553 1.112 -.306 20 CSM_TR .801 1.044 -.785 20 ECH3TR .174 1.501 -.649 20 ECH4TR .767 1.121 -.881 20 GFDLTR .719 .954 -.553 20 GISSTR .688 .799 .123 20 HAD2TR .920 .743 -.598 20 HAD3TR .923 .974 -.883 20 IAP_TR .599 1.408 -.734 20 LMD_TR .432 2.977 -2.103 20 MRI_TR .216 2.895 -2.026 20 PCM_TR .740 1.372 -1.041 20 MODBAR .813 .879 -.654 20
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What’s New (and Exciting)
• SCENGEN is being updated– Have IPCC AR4 models– 2.5o resolution– May have other bells and whistles
• Another very useful tool are the NCAR created PDFs
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Thank You!
I’d be happy to take questions