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Climate <br />City of Santa Ana -Park View at Town and Country Manor <br />Draft EIR <br />• A rise in sea levels resulting in the displacement of coastal businesses and residences. During <br />the past century, sea levels along California's coast have risen about seven inches. If heat - <br />trapping emissions continue unabated and temperatures rise into the higher warming range, sea <br />level is expected to rise an additional 22 to 35 inches by the end of the century. Elevations of <br />this magnitude would inundate coastal areas with salt water, accelerate coastal erosion, threaten <br />vital levees and inland water systems, and disrupt wetlands and natural habitats. <br />• Damage to marine ecosystems and the natural environment. <br />• An increase in infections, disease, asthma, and other health - related problems. <br />• A decrease in the health and productivity of California's forests. <br />Gases that trap heat in the atmosphere are referred to as greenhouse gases. The effect is analogous to <br />the way a greenhouse retains heat. Common greenhouse gases include water vapor, carbon dioxide, <br />methane, nitrous oxides, chlorofluorocarbons, hydrotluorocarbons, pertluorocarbons, sulfur <br />hexatluoride, ozone, and aerosols. Natural processes and human activities emit greenhouse gases. <br />The presence of greenhouse gases in the atmosphere affects the earth's temperature. Without the <br />natural heat trapping effect of greenhouse gas, the earth's surface would be about 340C cooler. <br />However, it is believed that emissions from human activities, such as electricity production and <br />vehicle use, have elevated the concentration of these gases in the atmosphere beyond the level of <br />naturally occurring concentrations. <br />The global warming potential (GWP) is the potential of a gas or aerosol to trap heat in the <br />atmosphere. Individual greenhouse gas compounds have varying GWP and atmospheric lifetimes. <br />Carbon dioxide, the reference gas for GWP, has a GWP of 1. The calculation of the carbon dioxide <br />equivalent is a consistent methodology for comparing greenhouse gas emissions since it normalizes <br />various greenhouse gas emissions to a consistent metric. Methane's warming potential of 21 <br />indicates that methane has a 21 times greater warming affect than carbon dioxide on a molecule per <br />molecule basis. A carbon dioxide equivalent is the mass emissions of an individual greenhouse gas <br />multiplied by its GWP. <br />Greenhouse gases that may be emitted by the project are summarized in Table 4.8 -1. <br />Table 4.8.1: Greenhouse Gases <br />reenh <br />a <br />Description and Physical Properties Sources <br />Carbon <br />Carbon dioxide is an odorless, colorless, natural <br />Natural sources include decomposition <br />dioxide (CO2) <br />greenhouse gas. Carbon dioxide's GWP is 1. <br />of dead organic matter; respiration of <br />The concentration in 2005 was 379 parts per <br />bacteria, plants, animals, and fungus; <br />million (ppm), which is an increase of about 1.4 <br />evaporation from oceans; and volcanic <br />ppm per year since 1960. Carbon dioxide from <br />outgassing. Anthropogenic sources are <br />fossil fuels contributed 81% of greenhouse gas <br />from burning coal, oil, natural gas, and <br />emissions in 2004 in California (CEC 2006). <br />wood. <br />4.8 -2 Michael Brandman Associates <br />H t(PN Rnb327b32700M%DEnib32700306ee01 Clvre Ch ged <br />