The <i>Fires, Asian, and Stratospheric Transport</i>–Las Vegas Ozone Study (<i>FAST</i>-LVOS)
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Published:2022-02-04
Issue:3
Volume:22
Page:1707-1737
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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:
Langford Andrew O., Senff Christoph J., Alvarez II Raul J., Aikin Ken C., Baidar Sunil, Bonin Timothy A., Brewer W. Alan, Brioude JeromeORCID, Brown Steven S., Burley Joel D., Caputi Dani J., Conley Stephen A.ORCID, Cullis Patrick D., Decker Zachary C. J., Evan StéphanieORCID, Kirgis Guillaume, Lin MeiyunORCID, Pagowski Mariusz, Peischl JeffORCID, Petropavlovskikh IrinaORCID, Pierce R. Bradley, Ryerson Thomas B.ORCID, Sandberg Scott P., Sterling Chance W., Weickmann Ann M., Zhang Li
Abstract
Abstract. The Fires, Asian, and Stratospheric Transport–Las Vegas Ozone Study (FAST-LVOS) was conducted in May and June of 2017 to
study the transport of ozone (O3) to Clark County, Nevada, a marginal
non-attainment area in the southwestern United States (SWUS). This 6-week (20 May–30 June 2017) field campaign used lidar, ozonesonde, aircraft, and
in situ measurements in conjunction with a variety of models to characterize
the distribution of O3 and related species above southern Nevada and
neighboring California and to probe the influence of stratospheric
intrusions and wildfires as well as local, regional, and Asian pollution on surface
O3 concentrations in the Las Vegas Valley (≈ 900 m above sea level, a.s.l.). In this paper, we describe the FAST-LVOS campaign and present
case studies illustrating the influence of different transport processes on
background O3 in Clark County and southern Nevada. The companion paper
by Zhang et al. (2020) describes the use of the AM4 and GEOS-Chem global
models to simulate the measurements and estimate the impacts of transported
O3 on surface air quality across the greater southwestern US and
Intermountain West. The FAST-LVOS measurements found elevated O3 layers above Las Vegas on more than 75 % (35 of 45) of the sample days and show that entrainment of these layers contributed to mean 8 h average regional
background O3 concentrations of 50–55 parts per billion by volume
(ppbv), or about 85–95 µg m−3. These high background
concentrations constitute 70 %–80 % of the current US National Ambient Air Quality Standard (NAAQS) of 70 ppbv (≈ 120 µg m−3 at 900 m a.s.l.) for the daily maximum 8 h average (MDA8) and will make attainment of the more stringent standards of 60 or 65 ppbv currently being considered
extremely difficult in the interior SWUS.
Funder
Climate Program Office
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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