Effects of urbanization on regional meteorology and air quality in Southern California
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Published:2019-04-05
Issue:7
Volume:19
Page:4439-4457
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Li Yun, Zhang JiachenORCID, Sailor David J.ORCID, Ban-Weiss George A.ORCID
Abstract
Abstract. Urbanization has a profound influence on regional meteorology and air quality
in megapolitan Southern California. The influence of urbanization on
meteorology is driven by changes in land surface physical properties and land
surface processes. These changes in meteorology in turn influence air quality
by changing temperature-dependent chemical reactions and emissions,
gas–particle phase partitioning, and ventilation of pollutants. In this study
we characterize the influence of land surface changes via historical
urbanization from before human settlement to the present day on meteorology and
air quality in Southern California using the Weather Research and Forecasting
Model coupled to chemistry and the single-layer urban canopy model
(WRF–UCM–Chem). We assume identical anthropogenic emissions for the
simulations carried out and thus focus on the effect of changes in land
surface physical properties and land surface processes on air quality.
Historical urbanization has led to daytime air temperature decreases of up to
1.4 K and evening temperature increases of up to 1.7 K. Ventilation of air
in the LA basin has decreased up to 36.6 % during daytime and increased
up to 27.0 % during nighttime. These changes in meteorology are mainly
attributable to higher evaporative fluxes and thermal inertia of soil from
irrigation and increased surface roughness and thermal inertia from
buildings. Changes in ventilation drive changes in hourly
NOx concentrations with increases of up to 2.7 ppb during
daytime and decreases of up to 4.7 ppb at night. Hourly O3
concentrations decrease by up to 0.94 ppb in the morning and increase by up
to 5.6 ppb at other times of day. Changes in O3 concentrations are
driven by the competing effects of changes in ventilation and precursor
NOx concentrations. PM2.5 concentrations show slight
increases during the day and decreases of up to 2.5 µg m−3
at night. Process drivers for changes in PM2.5 include modifications
to atmospheric ventilation and temperature, which impact gas–particle phase
partitioning for semi-volatile compounds and chemical reactions.
Understanding process drivers related to how land surface changes effect
regional meteorology and air quality is crucial for decision-making on urban
planning in megapolitan Southern California to achieve regional climate
adaptation and air quality improvements.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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