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SU0014502
Environmental Health - Public
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SU0014502
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Last modified
8/25/2022 10:29:54 AM
Creation date
11/4/2021 4:18:13 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0014502
PE
2675
FACILITY_NAME
PA-1900240
STREET_NUMBER
11000
Direction
N
STREET_NAME
WEST
STREET_TYPE
LN
City
LODI
Zip
95242-
APN
05908029, -07 -30
ENTERED_DATE
11/4/2021 12:00:00 AM
SITE_LOCATION
11000 N WEST LN
RECEIVED_DATE
5/2/2022 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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Administrative Draft Environmental Impact Report <br /> Gill Medical Center Project <br /> 4.5 AIR QUALITY <br /> This section evaluates the Project-related effects to air quality.This section is based on the Air Quality and <br /> Greenhouse Gas Emissions Assessment prepared by ECORP Consulting, Inc. (2020) (see Draft EIR <br /> Appendix D).The information provided below is an abridged version of this report.This analysis was <br /> prepared using methodologies and assumptions recommended by the San Joaquin Valley Air Pollution <br /> Control District (SJVAPCD) and California Air Resources Board (CARB). Regional and local existing <br /> conditions are presented, along with pertinent standards and regulations.The purpose of this assessment <br /> is to estimate Project-generated criteria air pollutant emissions attributable to the Project and to <br /> determine the level of impact the Project would have on the environment. <br /> 4.5.1 Environmental Setting <br /> 4.5.1.1 San Joaquin Valley Air Basin <br /> The California Air Resources Board (CARB) divides the state into air basins that share similar <br /> meteorological and topographical features.The San Joaquin Valley Air Basin (SJVAB) occupies the <br /> southern two-thirds of the Central Valley and includes the Project site. The SJVAB is mostly flat, less than <br /> 1,000 feet in elevation, and is surrounded on three sides by the Sierra Nevada, Tehachapi, and Coast <br /> Range mountains.This bowl-shaped feature forms a natural barrier to the dispersion (spreading over an <br /> area) of air pollutants. As a result, the SJVAB is highly susceptible to pollutant accumulation over time. <br /> Climate and Meteorology <br /> The climate in the SJVAB is strongly influenced by the presence of mountain ranges.The mountains create <br /> a partial rain shadow over the valley and block the free circulation of air, trapping stable air in the valley <br /> for extended periods.The climate is semi-arid and is characterized by long, hot, dry summers and cool, <br /> wet, and foggy winters. Based on historical data obtained from the meteorological station located in <br /> Bakersfield, ambient temperatures range from an average minimum of 39'F in January to an average <br /> maximum of 98°F in July.The average monthly precipitation is approximately 6.24 inches per year, with <br /> January and February averaging 1.35 inches. The average daily wind speed is 5.9 miles per hour (mph). <br /> The air flow patterns are characterized by one of four directions depending on the season. For example, <br /> during the summer, winds are predominantly northwestern (up valley), while winters typically feature a <br /> prevailing stagnant condition that leads to high incidence of valley fog. <br /> Atmospheric Stability and Inversions <br /> Stability describes the relative resistance of the atmosphere to vertical motion,which in turn mixes the air. <br /> The stability of the atmosphere is dependent on the vertical distribution of temperature with height. <br /> Unstable conditions often occur during daytime hours when solar heating warms the lower atmospheric <br /> layers while the upper layers remain cold. In contrast, an inversion is a layer of warmer air over a layer of <br /> cooler air. Inversions influence the mixing depth of the atmosphere, which is the vertical depth available <br /> for diluting air pollution near the ground.The SJVAB experiences both surface-based and elevated <br /> inversions.The shallow surface-based inversions can be present in the morning but are often broken by <br /> daytime heating of the air layers near the ground. The deep, elevated inversions occur less frequently than <br /> Air Quality 4.5-1 October 2021 <br />
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