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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 RTPAsA2This emission scenario represents a differentiated world <strong>in</strong> which economicgrowth is uneven and the <strong>in</strong>come gap rema<strong>in</strong>s large between now-<strong>in</strong>dustrializedand develop<strong>in</strong>g parts of the world; and people, ideas, and capital are less mobileso that technology diffuses more slowly. The underly<strong>in</strong>g theme is self-relianceand preservation of local identities. Fertility patterns across regions convergevery slowly, which results <strong>in</strong> cont<strong>in</strong>uously <strong>in</strong>creas<strong>in</strong>g population. Economicdevelopment is primarily <strong>regional</strong>ly oriented and per capita economic growthand technological <strong>change</strong> more fragmented and slower than other scenarios. Theemissions lie near the high end of the range of GHG emissions scenarios.B1This emissions scenario presents a future with a high level of environmental andsocial consciousness, comb<strong>in</strong>ed with a globally coherent approach to moresusta<strong>in</strong>able development. The B1 scenario assumes global population growthpeaks by mid-century and then decl<strong>in</strong>es, a rapid economic shift towards serviceand <strong>in</strong>formation economies, and the <strong>in</strong>troduction of clean and resource-efficienttechnologies. The emissions at the low end of the range of GHG emissionsscenarios.General Circulation ModelsGeneral circulation models (GCMs) are used for predict<strong>in</strong>g <strong>climate</strong> <strong>change</strong>. Theymodel how the atmosphere, oceans, land surface, and ice <strong>in</strong>teract to createweather and <strong>climate</strong> over long periods of time (decades and centuries) over thewhole globe. GCMs subdivide the Earth’s surface, atmosphere, and oceans <strong>in</strong>toa 3D grid of thousands of cells. Standard physical equations for the transfer ofheat, water, and momentum are solved for each grid cell to predict temperature,precipitation, and w<strong>in</strong>ds. Many relevant processes are well represented at thescale of these grid cells, such as the large-scale westerly flow of moisture fromthe Pacific Ocean. Many GCMs have been developed around the world; themost recent IPCC assessment report made use of projections from 24 differentGCMs.Cambridge Systematics, Inc. 3-9

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