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SR0082985_SSNL
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SR0082985_SSNL
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Entry Properties
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 4.5-1 <br />4.5 Greenhouse Gas Emissions <br />This section describes the existing greenhouse gas (GHG) conditions of the 14800 W. Schulte Road Logistics Center <br />(Project) site and vicinity, identifies associated regulatory requirements, evaluates potential impacts, and identifies <br />mitigation measures related to implementation of the Project. <br />In addition to the documents incorporated by reference (see Section 2.7 , Documents Incorporated by Reference, <br />of Chapter 2, Introduction, of this Environmental Impact Report), the following analysis is based, in part, on the <br />following sources: <br />• Air Quality and Greenhouse Gas Emissions Analysis Technical Report prepared by Dudek in January <br />2021 (Appendix B) <br />• Traffic Impact Analysis prepared by Advanced Mobility Group in Month 2020 (Appendix F) <br />4.5.1 Existing Conditions <br />Climate Change Overview <br />Climate change refers to any significant change in measures of climate, such as temperature, precipitation, or wind <br />patterns, lasting for an extended period of time (i.e., decades or longer). The Earth’s temperature depends on the <br />balance between energy entering and leaving the planet’s system. Many factors, both natural and human, can <br />cause changes in Earth’s energy balance, including variations in the sun’s energy reaching Earth, changes in the <br />reflectivity of Earth’s atmosphere and surface, and changes in the greenhouse effect, which affects the amount of <br />heat retained by Earth’s atmosphere (EPA 2017a). <br />The greenhouse effect is the trapping and build-up of heat in the atmosphere (troposphere) near the Earth’s <br />surface. The greenhouse effect traps heat in the troposphere through a threefold process as follows: Short-wave <br />radiation emitted by the Sun is absorbed by the Earth, the Earth emits a portion of this energy in the form of long - <br />wave radiation, and GHGs in the upper atmosphere absorb this long-wave radiation and emit it into space and <br />toward the Earth. The greenhouse effect is a natural process that contributes to regulating the Earth’s temperature <br />and creates a pleasant, livable environment on the Earth. Human activities that emit additional GHGs to th e <br />atmosphere increase the amount of infrared radiation that gets absorbed before escaping into space, thus <br />enhancing the greenhouse effect and causing the Earth’s surface temperature to rise (EPA 2017a). <br />The scientific record of the Earth’s climate shows that the climate system varies naturally over a wide range of time <br />scales and that, in general, climate changes prior to the Industrial Revolution in the 1700s can be explained by <br />natural causes, such as changes in solar energy, volcanic eruptions, and natu ral changes in GHG concentrations. <br />Recent climate changes, in particular the warming observed over the past century, however, cannot be explained <br />by natural causes alone. Rather, it is extremely likely that human activities have been the dominant cause of that <br />warming since the mid-twentieth century and is the most significant driver of observed climate change (IPCC 2013; <br />EPA 2017a). Human influence on the climate system is evident from the increasing GHG concentrations in the <br />atmosphere, positive radiative forcing, observed warming, and improved understanding of the climate system (IPCC <br />2013). The atmospheric concentrations of GHGs have increased to levels unprecedented in the last 800,000 years, <br />primarily from fossil fuel emissions and secondarily from emissions associated with land use changes (IPCC 2013).
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