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addressing climate change adaptation in regional transportation plans

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Cal-Adapt ProjectionsTable 25. Summary of Cal-Adapt Climate Projections for the Central Coast RegionEffectTemperatureChange,1990-2100PrecipitationHeat WaveSnowpackWildfire RiskRangesJanuary <strong>in</strong>crease <strong>in</strong> average temperatures: 1°F to 2°F <strong>in</strong> 2050 and 4°F to 5°F by 2100.July <strong>in</strong>crease <strong>in</strong> average temperatures: 2°F to 3°F by 2050 and 4°F to 7°F by 2100, with larger<strong>in</strong>creases <strong>in</strong> the mounta<strong>in</strong>ous regions to the east.(Modeled high temperatures – average of all models; high carbon emissions scenario)Low areas are projected to experience decl<strong>in</strong>es <strong>in</strong> annual precipitation ofabout 2 <strong>in</strong>ches by 2050 and 3 to 4 <strong>in</strong>ches, by 2100 while more elevatedareas are projected to experiences loses of approximately 10 <strong>in</strong>ches.(CCSM3 <strong>climate</strong> model; high carbon emissions scenario)Heat waves are def<strong>in</strong>ed as five days over 79°F to 85°F along the coast and 99°F to 101°F <strong>in</strong>land.Coastal areas should expect one more heat wave per year by 2050 and four to eight more peryear by 2100. Inland, three to four more heat waves are expected to 2050 and eight to tenmore per year <strong>in</strong> 2100.Snowpack <strong>in</strong> the eastern elevated regions is projected to decrease by approximately 9 <strong>in</strong>ches,result<strong>in</strong>g <strong>in</strong> pack that is less than 4 <strong>in</strong>ches by March 2090.(CCSM3 <strong>climate</strong> model; high carbon emissions scenario)The eastern edge of the region is projected to experience an<strong>in</strong>crease <strong>in</strong> wildfire risk of 4 to 6 times current conditions.(GFDL model, high carbon emissions scenario)[Public Interest Energy Research, 2011. Cal-Adapt. Retrieved from http://cal-adapt.org]Water SourcesExcept for the State Water Project, which derives from Sierra Nevada sources, most ofthe region’s water comes from the region itself. Overall, 66 percent of the region’s watercomes from groundwater, with the rema<strong>in</strong>der split mostly between federal projects andreuse. Only about 6 percent of the region’s total, mostly <strong>in</strong> San Luis Obispo and SantaBarbara counties, comes from the State Water Project (DWR, 2009). Federal projects (theU.S. Bureau of Reclamation’s Santa Maria and Cachuma projects) store floodwater fromthe Santa Maria River watersheds, us<strong>in</strong>g it to replenish groundwater and mitigate saltwater<strong>in</strong>trusion. The region’s water supply <strong>in</strong> 2005 totaled approximately 1.4 million acre-feet, lessthan 1 percent of which came from outside regions. Agriculture accounted for the majorityof use at about 0.9 million acre-feet, followed by urban use at 0.25 million acre-feet. Totalreservoir storage capacity <strong>in</strong> the region is 1.23 million acre-feet (DWR, 2009).PAGE 66APG: UNDERSTANDING REGIONAL CHARACTERISTICS

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