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• <br /> r <br /> • Draft Supplemental Environmental Impact Report Page IV.D-2 <br /> Forward Inc. Landfill 2018 Revised Project <br /> • result, the SJVAB is highly susceptible to pollutant accumulation over time. Frequent transport <br /> • of pollutants into the SJVAB from upwind sources also negatively contributes to air quality. <br /> Wind speed and direction play an important role in dispersion and transport of air pollutants. <br /> • During summer periods, winds usually originate from the north end of the San Joaquin Valley <br /> • and flow in a south-southeasterly direction through the valley,through the Tehachapi pass and <br /> • into the neighboring Southeast Desert Air Basin. During winter months, winds occasionally <br /> originate from the south end of the valley and flow in a north-northwesterly direction. Also, <br /> during winter months, the valley experiences light, variable winds, less than 10 miles per hour <br /> • (mph). Low wind speeds, combined with low inversion layers in the winter, create a climate <br /> • conducive to high concentrations of certain air pollutants. <br /> The SJVAB has an inland Mediterranean climate that is characterized by warm, dry summers <br /> and cooler winters. Summer high temperatures often exceed 100 degrees Fahrenheit (°F), <br /> averaging from the low 90s in the northern part of the valley to the high 90s in the south. The <br /> • daily summer temperature variation can be as high as 30 degrees °F. Winters are for the most <br /> part mild and humid. Average high temperatures during the winter are in the 50s, while the <br /> average daily low temperature is approximately 45 degrees°F. Precipitation in the Stockton <br /> • area falls almost exclusively from mid-November to mid-April from the fringes of mid-latitude <br /> • storms. The Stockton area averages 13.5 inches of rain annually. <br /> The vertical dispersion of air pollutants in the valley is limited by the presence of persistent <br /> temperature inversions. Air temperatures usually decrease with an increase in altitude. A <br /> • reversal of this atmospheric state, where the air temperature increases with height, is termed an <br /> inversion. Air above and below an inversion does not mix because differences in air density <br /> thereby restrict air pollutant dispersal. <br /> • Regulatory Framework <br /> Air quality issues are under the jurisdiction of the United States Environmental Protection <br /> Agency (EPA), the California Air Resources Board (CARB), and the SJVAPCD. Regulation of <br /> air pollution is achieved through both Federal and State ambient air quality standards and <br /> • emission limits for individual sources of air pollutants. An"ambient air quality standard" <br /> • represents a level of an air pollutant in the outdoor (ambient) air that is necessary to protect <br /> public health. The ambient standards do not apply to indoor environments. <br /> . Again, as required by the federal Clean Air Act (CAA), the EPA identified criteria pollutants <br /> . and established National Ambient Air Quality Standards (NAAQS, or national standards) to <br /> protect the public health and welfare. There are NAAQS for ozone (03), carbon monoxide <br /> (CO), nitrogen dioxide (NOA sulfur dioxide (SO2), respirable particulate matter equal to or less <br /> than 10 microns in diameter(PM,o), fine particulate matter equal to or less than 2.5 microns in <br /> • diameter(PM2,5), and lead (Pb). These pollutants are known as "criteria" air pollutants because <br /> • standards have been established to meet specific public health and welfare criteria. <br /> The NAAQS are defined as the maximum acceptable concentration that may be reached,but <br /> not exceeded more than once per year. California has adopted more stringent ambient air <br />