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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 RTPAsexample, bridges), or based on other criteria important to the region. The <strong>climate</strong>data accompany<strong>in</strong>g this report has been provided for the follow<strong>in</strong>g periods:Present conditions. Climate <strong>in</strong>formation for present conditions refers to datareflect<strong>in</strong>g the current status of a given <strong>climate</strong> stressor. Data for presentconditions will be used as the basel<strong>in</strong>e to which future time horizons arecompared and the magnitude of <strong>change</strong> will be ascerta<strong>in</strong>ed. Typically,present conditions stressor levels are calculated as historic average overmultiple years (i.e., 1970-1999).Future conditions. Future <strong>climate</strong> projections are often averaged overmultiple years to reduce the spread of year-to-year variability and reflect thegeneral trend of expected <strong>change</strong>s. Typically, projection periods are divided<strong>in</strong>to equal <strong>in</strong>tervals for <strong>climate</strong> trend averag<strong>in</strong>g such as decadal averages or30-year averages. As such, the <strong>climate</strong> conditions for future analysis yearsshould represent an average of the <strong>climate</strong> trend over a period of severalyears around the time period selected.Identify Stressor Types and ThresholdsIn this context, the term “<strong>climate</strong> stressors” refers to <strong>climate</strong> conditions that posepotential hazards to <strong>transportation</strong> assets, many of which are projected to<strong>in</strong>crease <strong>in</strong> frequency or severity <strong>in</strong> the future. Examples of <strong>climate</strong> stressors<strong>in</strong>clude temperature, precipitation, and sea-level rise. Geospatial <strong>climate</strong>datasets can be used to aid <strong>in</strong> characteriz<strong>in</strong>g the magnitude of <strong>change</strong> <strong>in</strong> thesestressors, enabl<strong>in</strong>g an analysis of the vulnerability of critical <strong>transportation</strong> assetsto these <strong>change</strong>s. Potential stressor impacts on <strong>transportation</strong> assets may<strong>in</strong>clude:Temperature. A primary variable affect<strong>in</strong>g <strong>transportation</strong> asset vulnerabilityis the average number of high heat days occurr<strong>in</strong>g with<strong>in</strong> a given year. Forexample, exposure to high temperatures can degrade the material strength ofb<strong>in</strong>d<strong>in</strong>g materials <strong>in</strong> asphalt and may leave roads vulnerable to damage.Quantify<strong>in</strong>g the number of heat days <strong>in</strong> a given region under exist<strong>in</strong>g andfuture conditions will aid <strong>in</strong> identify<strong>in</strong>g the regions and assets most likely tobe impacted by ris<strong>in</strong>g temperatures.Precipitation. Design of dra<strong>in</strong>age capacity for <strong>transportation</strong> assets relies onknowledge of return periods for ra<strong>in</strong>fall and streamflow conditionsestablished over years of historical measured data. Climate projections<strong>in</strong>dicate that extreme precipitation events are likely to <strong>in</strong>crease <strong>in</strong> frequencyand severity, which may alter the expected return period of a given ra<strong>in</strong>falldepth or streamflow peak. Knowledge of expected <strong>change</strong>s <strong>in</strong> precipitation,and associated hydrologic variables <strong>in</strong>clud<strong>in</strong>g snowpack, runoff, andbaseflow, will be critical for evaluat<strong>in</strong>g the vulnerability of dra<strong>in</strong>age systemsfor various <strong>transportation</strong> assets.Sea-Level Rise. Impacts to <strong>transportation</strong> assets from extreme tide levels,exacerbated by net <strong>in</strong>creases <strong>in</strong> sea level, <strong>in</strong>clude the <strong>in</strong>creased frequency,extent, and depth of <strong>in</strong>undation. Sea-level rise is also expected to <strong>in</strong>crease the10-4 Cambridge Systematics, Inc.

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