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addressing climate change adaptation in regional transportation plans

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Address<strong>in</strong>g Climate Change Adaptation <strong>in</strong> Regional Transportation PlansA Guide for California MPOs and RTPAsMore <strong>in</strong>tense precipitation may cause an <strong>in</strong>creased <strong>in</strong>cidence of flood<strong>in</strong>g alongcoastal roadways and rail l<strong>in</strong>es. Low-ly<strong>in</strong>g bridge and tunnel entrances for railand rail transit will also be more susceptible to flood<strong>in</strong>g, and thousands ofculverts and other dra<strong>in</strong>age <strong>in</strong>frastructure could be undersized—designed fortoday’s precipitation <strong>in</strong>stead of tomorrow’s. 7The cycle of landslides closely follows the ra<strong>in</strong>fall <strong>in</strong>tensity <strong>in</strong> the w<strong>in</strong>ter months.Repeated periods of high-<strong>in</strong>tensity ra<strong>in</strong>fall often result <strong>in</strong> landslides throughoutthe State, result<strong>in</strong>g <strong>in</strong>, among other th<strong>in</strong>gs, closures of roads, rail l<strong>in</strong>es, and other<strong>transportation</strong> systems. For example, the recurrence of the La Conchita landslideroughly every 10 years is caused by w<strong>in</strong>ter storms that, <strong>in</strong> the last failure,completely closed Highway 101 and the parallel rail corridor for a week (CNRA2012).Chang<strong>in</strong>g precipitation could result <strong>in</strong> erosion and subsidence of <strong>transportation</strong><strong>in</strong>frastructure like rail beds, caus<strong>in</strong>g the <strong>in</strong>terruption or disruption of traffic. Thechang<strong>in</strong>g precipitation (for <strong>in</strong>stance, <strong>change</strong>s from frozen to liquid precipitation)could <strong>change</strong> runoff patterns, <strong>in</strong>creas<strong>in</strong>g the risk of floods, landslides, slopefailures, and consequent damage to roadways and rail beds, especially ruralareas <strong>in</strong> the w<strong>in</strong>ter and spr<strong>in</strong>g months. 8Impacts of Chang<strong>in</strong>g Temperature on the RegionalTransportation SystemCalifornia should expect overall hotter conditions by the end of the century. Allmodel projections suggest <strong>in</strong>creased temperatures, with the level of emissionsrepresent<strong>in</strong>g the biggest uncerta<strong>in</strong>ty: temperature levels will rise more quicklyand be higher by the end of this century with higher emissions.Changes <strong>in</strong> temperature may damage materials used <strong>in</strong> roads and other<strong>transportation</strong> <strong>in</strong>frastructure. The <strong>in</strong>crease <strong>in</strong> average temperature will also havea cumulative impact on the material properties of <strong>in</strong>frastructure systems.Individual days of extreme temperatures can also produce failures. Typicalconstruction materials degrade <strong>in</strong> extreme heat, cold, and moisture. An <strong>in</strong>crease<strong>in</strong> the <strong>in</strong>tensity of these elements will result <strong>in</strong> more rapid degradation of analready aged <strong>in</strong>frastructure.Chang<strong>in</strong>g temperature may affect <strong>in</strong>creased freeze-thaw conditions, creat<strong>in</strong>gfrost heaves and potholes on road and bridge surfaces and compromis<strong>in</strong>g railbeds. Longer periods of extreme heat can cause deformation of asphalt and rails,<strong>in</strong>creas<strong>in</strong>g the chance of derailments, or at a m<strong>in</strong>imum, requir<strong>in</strong>g speed7 Ibid.8 Ibid.Cambridge Systematics, Inc. 4-9

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