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SR0082985_SSNL
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SR0082985_SSNL
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Last modified
2/10/2022 11:04:15 AM
Creation date
12/21/2020 3:02:11 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0082985
PE
2602
STREET_NUMBER
14800
Direction
W
STREET_NAME
SCHULTE
STREET_TYPE
RD
City
TRACY
Zip
95377
APN
20924023
ENTERED_DATE
12/8/2020 12:00:00 AM
SITE_LOCATION
14800 W SCHULTE RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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4.5 – Greenhouse Gas Emissions <br />Draft Environmental Impact Report February 2021 <br />14800 W. Schulte Road Logistics Center 4.5-5 <br />As outlined in Table 4.5-2, the County of San Joaquin’s Greenhouse Gas Emissions by Sectors (2007), the County <br />of San Joaquin (County) emitted 3,051,996 MT CO2e in 2007 (County of San Joaquin 2014). <br />Table 4.5-2. County of San Joaquin Greenhouse Gas Emissions by Sectors (2007) <br />Source Category Annual GHG Emissions (MT CO2e) <br />Electricity 831,532 <br />Transportation 1,350,924 <br />Waste 41,067 <br />Wastewater 2,784 <br />Agriculture 825,689 <br />Total 3,051,996 <br />Source: County of San Joaquin 2014. <br />Notes: GHG = greenhouse gas; MT CO2e = metric tons of carbon dioxide equivalent. <br />Reflects inventory year 2007. <br />Total may not add due to rounding. <br />Potential Effects of Climate Change <br />In California, climate change impacts have the potential to affect sea-level rise, agriculture, snowpack and water <br />supply, forestry, wildfire risk, public health, and electricity demand and supply. The primary effect of global climate <br />change has been a rise in average global tropospheric temperature. Reflecting the long-term warming trend since <br />pre-industrial times, observed mean surface temperature for the decade 2006–2015 was 0.87°C (likely between <br />0.75°C and 0.99°C) higher than the average over the 1850–1900 period (IPCC 2018). Scientific modeling predicts <br />that continued emissions of GHGs at or above current rates would induce more extreme climate changes during <br />the twenty-first century than were observed during the twentieth century. Human activities are estimated to have <br />caused approximately 1.0°C (1.8°F) of global warming above pre-industrial levels, with a likely range of 0.8°C to <br />1.2°C (1.4°F to 2.2°F) (IPCC 2018). Global warming is likely to reach 1.5°C (2.7°F) between 2030 and 2052 if it <br />continues to increase at the current rate (IPCC 2018). <br />Although climate change is driven by global atmospheric conditions, climate change impacts are felt locally. A <br />scientific consensus confirms that climate change is already affecting California. The Office of Environmental Health <br />Hazard Assessment identified various indicators of climate change in California, which are scientifically based <br />measurements that track trends in various aspects of climate change. Many indicators reveal discernible evidence <br />that climate change is occurring in California and is having significant, measurable impacts in the s tate. Changes <br />in the state’s climate have been observed, including an increase in annual average air temperature , with record <br />warmth from 2012 to 2016; more frequent extreme heat events; more extreme drought; a decline in winter chill; <br />an increase in cooling degree days and a decrease in heating degree days; and an increase in variability of statewide <br />precipitation (OEHHA 2018). <br />Warming temperatures and changing precipitation patterns have altered California’s physical systems—the ocean, <br />lakes, rivers, and snowpack—upon which the state depends. Winter snowpack and spring snowmelt runoff from the <br />Sierra Nevada and southern Cascade Mountains provide approximately one-third of the state’s annual water supply. <br />Impacts of climate on physical systems have been observed, such as high variability of snow -water content (i.e., <br />amount of water stored in snowpack), decrease in snowmelt runoff, glacier change (loss in area), rise in sea levels, <br />increase in average lake water temperature and coastal ocean temperature, and a decrease in dissolved oxygen in <br />coastal waters (OEHHA 2018).
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