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ClimateChange Assessment Guide.pdf - University of Waterloo

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<strong>Guide</strong> for <strong>Assessment</strong> <strong>of</strong> Hydrologic Effects <strong>of</strong> Climate Change in Ontario80Scenarios can be sorted according to annual simulatedchanges in air temperature and total precipitation. Thescenarios associated with the percentiles <strong>of</strong> interestin the Percentile Method (Section 6.4.3.2) can bedetermined from these sorted groupings.The meteorological inputs to the hydrology model canbe adjusted to reflect the simulated change fields on amonth by month basis for each scenario selected. Thesemonthly change fields represent average changes in theclimate parameter and are applied to each value in theinput data time series. This process changes the meanvalues for the time series but will not affect the variabilityor frequency <strong>of</strong> occurrence <strong>of</strong> extreme conditions. It is,therefore, not suitable for assessments that focus onpeak flow and flooding issues.While most hydrologic models and climate changeimpact assessments focus on the effects <strong>of</strong> airtemperature and precipitation, other meteorologicalparameters may be required. Models such as HSP-F canuse solar radiation and wind speed to simulate snowpackbehaviour and to modify evapotranspiration. Hydrologicmodels are not as sensitive to wind and solar radiationas they are to temperature or precipitation; therefore,this aspect <strong>of</strong> future climates is <strong>of</strong> lesser importance. Forthis reason, the GCM change field method is generallyadequate for adjusting these parameters for use inclimate change impact assessments. This is also true inassessments involving downscaled climates.<strong>Assessment</strong> <strong>of</strong> climate impacts is discussed in Section6.6. Examples <strong>of</strong> studies conducted in Ontario using thechange field method and typical change field values arediscussed in Section 5.1.6.5.3 Statistical Downscaling MethodVarious statistical downscaling models are currentlyavailable for climate downscaling. The StatisticalDownscaling Model (SDSM) is one tool that is availableon the Environment Canada website (www.cccsn.ca). Thismodel was developed in the UK by Drs. R. Wilby and C.Dawson. It is a hybrid <strong>of</strong> a stochastic weather generatorand a regression-based downscaling method, packagedwith a user friendly Windows interface. The modelallows users to generate single site scenarios <strong>of</strong> dailyweather variables (i.e., air temperature and precipitation)for current and future climates. SDSM helps the useridentify large scale predictors (i.e., mean sea levelpressure, surface vorticity or specific humidity) thatexplain much <strong>of</strong> the climate variability at a site. Statisticalmodels are built using these predictors to estimate thepredictand values. Predictands are the local climatevariables <strong>of</strong> interest (i.e., temperature and precipitation).As predictors tend to change in the future, so toowill the simulated predictands, through the statisticalrelationships determined by the model.Guidance:To examine climate variability, at least onestatistical downscaling model scenario should beapplied to develop future climates. The GCMemissionscenario used in the climate simulationshould match one <strong>of</strong> the scenarios chosen for thesuite <strong>of</strong> GCM-emission scenarios, if possible.The SDSM application process requires predictor timeseries for current and future conditions. For currentconditions, predictor time series are created from theGCM runs, available at GCM grid points using the NCEP(National Centre for Environmental Prediction) model.NCEP is a reanalysis <strong>of</strong> recent weather that creates aretrospective accounting <strong>of</strong> the atmospheric conditionsbased on observed data. In effect, the NCEP runs fillin values for a wide variety <strong>of</strong> predictors by modellingexisting and recent conditions. A large number <strong>of</strong> NCEPvariables are available for all <strong>of</strong> North America for theperiod 1961 to 1990.GCM-based runs that extend well into the future(typically to 2100) provide the predictor time series forfuture emission scenarios, for various time horizons(i.e., 2050s, 2070s etc.). The local climate predictandsare generated using the same statistical relationshipsbetween the predictors and predictands developed forcurrent conditions.To acquire a downloaded copy <strong>of</strong> SDSM with the user’smanual as well as a brief summary <strong>of</strong> the modellingprocess, visit the Environment Canada website, www.CCCSN.ca. Click Downscaling Tools on the left handside <strong>of</strong> the screen and select SDSM from the drop downmenu. Review the summary version <strong>of</strong> model applicationand refer to the full version <strong>of</strong> the manual for detaileddescriptions and a well documented example for

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