11.07.2015 Views

ClimateChange Assessment Guide.pdf - University of Waterloo

ClimateChange Assessment Guide.pdf - University of Waterloo

ClimateChange Assessment Guide.pdf - University of Waterloo

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Climate Change <strong>Assessment</strong>65Guidance:Scenario runs should use the 2050s time horizonif resources limit the assessment to one timeperiod.The 2050s time horizon is far enough in the future thatthe changes in climate are likely to be sufficiently largeto see notable impacts emerge. This time frame isappropriate for both a strategic planning approach anda risk framing and assessment approach in which theimpact assessment information is used to build resiliencein the system or expand the coping range throughadaptation. At this point in the future, the climate systemresponse to the different emission scenarios is beginningto diverge. Also, the most recent RCM output is currentlyonly available for the 2040 to 2070 period.The 2020s time horizons are used for numerous planninginitiatives; however, we do not recommend using thistime period as the only climate change scenario. Thistime period is not as likely to produce large changes inclimate and hence produce potential climate changeimpacts. It may be useful, however, for establishing anintermediate assessment <strong>of</strong> potential impacts, as theemission scenarios remain relatively similar throughoutthe 2020s period; and for informing the development <strong>of</strong>an impact monitoring program and for indicating whenadaptations may need to be implemented.The 2080s period is useful for long-term strategicplanning; some municipalities and agencies areundertaking 100-year planning exercises (e.g., GreatVancouver District) where incorporating this climateimpact information would be warranted.6.4.3 Selecting the Number <strong>of</strong> Climate ChangeScenariosGuidance:The IPCC recommends that users shouldapply multiple climate change scenarios – asmany as possible - in impacts and adaptationassessments.From the knowledge-generating perspective, thechallenge remains determining how many scenariosshould be used to gain understanding <strong>of</strong>:• The potential range <strong>of</strong> impacts that may occur;• The potential effects that may be outside currentconditions or the coping range;• The range <strong>of</strong> risks; and• The range <strong>of</strong> future conditions that adaptationstrategies should accommodate to build resilience/robustness in watersheds.Practical considerations also exist when choosing thenumber <strong>of</strong> scenarios; they include the following:• The capabilities <strong>of</strong> those undertaking the impactassessment to incorporate a large number <strong>of</strong>scenarios into the modelling process. This includesthe availability <strong>of</strong> tools to manipulate and analyze thelarge amounts <strong>of</strong> data generated.• Interpreting and explaining the results generatedfrom multiple scenarios for those who must integratethe climate change impact assessment informationinto the decision making and policy making process.This section explores two candidate approaches forshort-listing climate change scenarios. This follows theoriginal screening for the case study that identified 57GCM- GHG combinations as candidates for developinginto climate change scenarios for hydrologic assessment.The proposed approaches include:• The scatter plot method - ‘bounding the uncertainty’(4 candidate scenarios); and• The percentile method (maximum 10 candidatescenarios).The initial screening <strong>of</strong> the GCM-GHG climate scenariosused in the <strong>Guide</strong>, as outlined in Section 6.4.2 above,focused on the availability <strong>of</strong> parameters that arecritical for hydrologic modelling. Thirty-nine <strong>of</strong> 57 futureclimates had monthly change fields for temperature,precipitation, wind speed and solar radiation (ID 1 to 39).Eighteen additional future climates were included eventhough there were no wind speed change field data (ID40 to 57). These additional future climates incorporatea broader range <strong>of</strong> GCMs (i.e., HadCM3 A2 informationthat could be linked to downscaling efforts that werebeing considered as part <strong>of</strong> the scenarios package).

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!