addressing climate change adaptation in regional transportation plans
addressing climate change adaptation in regional transportation plans addressing climate change adaptation in regional transportation plans
Cal-Adapt ProjectionsTable 13. Summary of Cal-Adapt Climate Projections for Northern Central ValleyEffectTemperatureChange, 1990-2100PrecipitationHeat WaveWildfire RiskRangesJanuary increase in average temperature of 4°F to 6°F and between8°F and 12°F by 2100.July increase in average temperature of 6°F to 7°F in 2050 and 12°Fto 15°F by 2100.(Modeled high temperatures – average of all models; high carbonemissions scenario)Annual precipitation is projected to decline by approximately one totwo inches by 2050 and three to six inches by 2100.(CCSM3 climate model; high carbon emissions scenario)Heat wave is defined as five days over 102°F to 105°F, except in themountainous areas to the east. Two to three more heat waves peryear are expected by 2050 with five to eight more by 2100.By 2085, the north and eastern portions of the region willexperience an increase in wildfire risk, more than 4 times currentlevels in some areas.(GFDL model, high emissions scenario)[Public Interest Energy Research, 2011. Cal-Adapt. Retrieved from http://cal-adapt.org]Water SourcesTwo rivers, the San Joaquin and Sacramento, run through this region. The riversoriginate from snowmelt in the Sierra Nevada and the mountainous regions inthe north and flow toward San Francisco Bay, where the flows eventually reachthe Pacific Ocean. The confluence of the rivers occurs in the Sacramento-SanJoaquin Delta.Water moves through the region through natural waterways as well as a networkof canals and reservoirs. The reservoir and canal systems that hold much of theregion’s water allow it to be leveraged for energy generation and recreationaluse (DWR, 2009). The water supply network for the region is highly complex.One third of the regional water supply relies on groundwater pumping, whichcan increase during drought periods when more water may be pumped to makeup for surface water shortfalls. For the remaining majority of the water supply,there is heavy reliance on the surface water conveyance systems that provide theinflow to the Sacramento-San Joaquin Delta (also known as the California Deltaor the Bay-Delta.The Delta serves as a primary water source for the entire state, servingapproximately 25 million residents as far south as San Diego and an agriculturalindustry valued at over $25 billion (San Diego County Water Authority, n.d.).These supplies are delivered through the State Water Project, the Central ValleyAPG: UNDERSTANDING REGIONAL CHARACTERISTICS PAGE 38
Project, and a host of other federal water projects. In the Delta, the system ofcanals, bordered by levees, also serves to deliver floodwater, support commercialfishing, provide for recreational activities, and maintain ecosystem health. Thenetwork of reservoirs within the region also plays a vital role in preventingsaltwater intrusion in the California Delta by providing freshwater flushes duringthe summer and fall (DWR, 2009).The Northern Central Valley region overlaps three hydrologic regions as definedby the Department of Water Resources: San Joaquin River, Sacramento River, andSacramento-San Joaquin Delta. Reservoir storage capacity in the SacramentoRiver and San Joaquin River hydrologic regions is 16.15 and 11.48 million acrefeet,respectively (DWR, 2009).Biophysical CharacteristicsWhile elevations range from 3,000 to 12,000 feet in the eastern areas of Madera,Butte, Sutter, and Tehama counties, areas located within the primary Delta zonein southern Yolo County and eastern Sacramento and San Joaquin counties are ator below sea level (CDFG, 2007). On average, elevation in the Northern CentralValley region is less than 300 feet above sea level. The region is bordered bythe Sierra Nevada to the east and the coastal mountain ranges to the west. Theextensive natural vegetation in the region is dominated by grasslands and scrubbut also contains hardwood and coniferous forest and woodland (FRAP, 1998).Major rivers include the Sacramento, San Joaquin, Feather, Merced, and Stanislaus.Many of the large lakes in the region are the result of river damming as part ofreservoir and water project construction.Regional Entities• Air Districts: Butte, Colusa, Feather River, Glenn, San Joaquin Valley Unified,Tehama, Yolo-Solano• Regional Organizations: Butte County Association of Governments,Tehama County Transportation Commission, Glenn County TransportationCommission, Colusa County Transportation Commission, Sacramento AreaCouncil of Governments, San Joaquin Council of Governments, StanislausCouncil of Governments (StanCOG), Merced County Association ofGovernments, Madera County Transportation Commission• Tribal Lands (U.S. EPA, 2011): Berry Creek, Colusa (Cachil Dehe), Cortina,Enterprise, Grindstone Creek, Mooretown, North Fork, Picayune, RumseyPAGE 39APG: UNDERSTANDING REGIONAL CHARACTERISTICS
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Cal-Adapt ProjectionsTable 13. Summary of Cal-Adapt Climate Projections for Northern Central ValleyEffectTemperatureChange, 1990-2100PrecipitationHeat WaveWildfire RiskRangesJanuary <strong>in</strong>crease <strong>in</strong> average temperature of 4°F to 6°F and between8°F and 12°F by 2100.July <strong>in</strong>crease <strong>in</strong> average temperature of 6°F to 7°F <strong>in</strong> 2050 and 12°Fto 15°F by 2100.(Modeled high temperatures – average of all models; high carbonemissions scenario)Annual precipitation is projected to decl<strong>in</strong>e by approximately one totwo <strong>in</strong>ches by 2050 and three to six <strong>in</strong>ches by 2100.(CCSM3 <strong>climate</strong> model; high carbon emissions scenario)Heat wave is def<strong>in</strong>ed as five days over 102°F to 105°F, except <strong>in</strong> themounta<strong>in</strong>ous areas to the east. Two to three more heat waves peryear are expected by 2050 with five to eight more by 2100.By 2085, the north and eastern portions of the region willexperience an <strong>in</strong>crease <strong>in</strong> wildfire risk, more than 4 times currentlevels <strong>in</strong> some areas.(GFDL model, high emissions scenario)[Public Interest Energy Research, 2011. Cal-Adapt. Retrieved from http://cal-adapt.org]Water SourcesTwo rivers, the San Joaqu<strong>in</strong> and Sacramento, run through this region. The riversorig<strong>in</strong>ate from snowmelt <strong>in</strong> the Sierra Nevada and the mounta<strong>in</strong>ous regions <strong>in</strong>the north and flow toward San Francisco Bay, where the flows eventually reachthe Pacific Ocean. The confluence of the rivers occurs <strong>in</strong> the Sacramento-SanJoaqu<strong>in</strong> Delta.Water moves through the region through natural waterways as well as a networkof canals and reservoirs. The reservoir and canal systems that hold much of theregion’s water allow it to be leveraged for energy generation and recreationaluse (DWR, 2009). The water supply network for the region is highly complex.One third of the <strong>regional</strong> water supply relies on groundwater pump<strong>in</strong>g, whichcan <strong>in</strong>crease dur<strong>in</strong>g drought periods when more water may be pumped to makeup for surface water shortfalls. For the rema<strong>in</strong><strong>in</strong>g majority of the water supply,there is heavy reliance on the surface water conveyance systems that provide the<strong>in</strong>flow to the Sacramento-San Joaqu<strong>in</strong> Delta (also known as the California Deltaor the Bay-Delta.The Delta serves as a primary water source for the entire state, serv<strong>in</strong>gapproximately 25 million residents as far south as San Diego and an agricultural<strong>in</strong>dustry valued at over $25 billion (San Diego County Water Authority, n.d.).These supplies are delivered through the State Water Project, the Central ValleyAPG: UNDERSTANDING REGIONAL CHARACTERISTICS PAGE 38