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ClimateChange Assessment Guide.pdf - University of Waterloo

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E-26<strong>Guide</strong> for <strong>Assessment</strong> <strong>of</strong> Hydrological Effects <strong>of</strong> Climate Change in OntarioMean Annual Precipitation Change (%)20.015.010.05.00.0-5.0Future Climates Selected byPercentile MethodFuture Climates Selected forDownscaling-10.01.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0Mean Annual Temperature Change ( o C)BCM2.0 - SR-A2BCM2.0 - SR-A1BBCM2.0 - SR-B1CGCM3T47(Run1) - SR-A2CGCM3T47(Run1) - SR-A1BCGCM3T47(Run1) - SR-B1CGCM3T63 - SR-A1BCGCM3T63 - SR-B1CNRMCM3 - SR-A2CNRMCM3 - SR-A1BCNRMCM3 - SR-B1CSIROMk3 - SR-A2CSIROMk3 - SR-A1BCSIROMk3 - SR-B1ECHAM5OM - SR-A2ECHAM5OM - SR-A1BECHAM5OM - SR-B1ECHO-G - SR-A2ECHO-G - SR-A1BECHO-G - SR-B1FGOALS-g1.0 - SR-A1BFGOALS-g1.0 - SR-B1GFDLCM2.0 - SR-A2GFDLCM2.0 - SR-A1BGFDLCM2.0 - SR-B1GFDLCM2.1 - SR-A2GFDLCM2.1 - SR-A1BGFDLCM2.1 - SR-B1GISSAOM - SR-A1BGISSAOM - SR-B1GISSE-H - SR-A1BGISSE-R - SR-A2GISSE-R - SR-B1HADCM3 - SR-A2HADCM3 - SR-A1BHADCM3 - SR-B1HadGEM1 - SR-A2HadGEM1 - SR-A1BINMCM3.0 - SR-A2INMCM3.0 - SR-A1BINMCM3.0 - SR-B1IPSLCM4 - SR-A2IPSLCM4 - SR-A1BIPSLCM4 - SR-B1MIROC3.2 hires - SR-A1BMIROC3.2 hires - SR-B1MIROC3.2 medres - SR-A2MIROC3.2 medres - SR-B1MIROC3.2 medres - SR-A1BMRI CGCM2.3.2a - SR-A2MRI CGCM2.3.2a - SR-A1BMRI CGCM2.3.2a - SR-B1NCARCCSM3 - SR-A2NCARCCSM3 - SR-A1BNCARCCSM3 - SR-B1NCARPCM - SR-A2NCARPCM - SR-A1BCGCM3T47(Run4) - SR-A2CGCM3T47(Run4) - SR-A1BFigure 4-1: Mean Annual Temperature and Precipitation Changes for Subwatershed 19 GCM Scenarios. Application <strong>of</strong> the Statistical Downscaling Model (SDSM) to downscaling local climates requires daily GCM simulatedpredictors for the selected SRES scenarios. As a reminder, the regression based statistical downscaling methods relyupon the development <strong>of</strong> statistical models that correlate predictand values with predictor values for a particularscenario and time horizon. Predictors from future time horizons are used to generate future predictand time series. Inthis application, downscaled air temperature and precipitation are required. It is possible to downscale otherparameters such as solar radiation and wind speed; however, hydrologic modelling is not sensitive to extremes withinthese time series and so future versions <strong>of</strong> these parameters can be developed using the change field method.The first step in developing statistically based climates using SDSM is to acquire the predictor time series for selectedscenarios from the Canadian Climate Change Scenarios Network website (www.CCCSN.ca). Under theDownscaling Tools menu, the Statistical Downscaling Input contains three choices for the SDSM and ASDPredictors. It is recommended that the latest CGCM3 Predictors be chosen. Once selected, the user is prompted toregister with the OURANOS website Data Access Integration (DAI) page. The site <strong>of</strong>fers data from the historic timeseries and the IPCC A2 and A1B experiments. Only the 4 th members (i.e., Run 4) <strong>of</strong> these experiments are available.Four datasets are <strong>of</strong>fered. Three <strong>of</strong> these are required for this study, namely:

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