Volatile organic compounds and ozone in Rocky Mountain National Park during FRAPPÉ
-
Published:2019-01-14
Issue:1
Volume:19
Page:499-521
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Benedict Katherine B., Zhou Yong, Sive Barkley C.ORCID, Prenni Anthony J., Gebhart Kristi A., Fischer Emily V., Evanoski-Cole Ashley, Sullivan Amy P., Callahan Sara, Schichtel Bret A.ORCID, Mao Huiting, Zhou Ying, Collett Jr. Jeffrey L.ORCID
Abstract
Abstract. The 2014 Front Range Air Pollution and Photochemistry
Éxperiment (FRAPPÉ) aimed to better characterize summertime air
quality in the Northern Front Range Metropolitan Area (NFRMA) and its impact
on surrounding areas. As part of this study, measurements of
gas- and particle-phase species were collected in Rocky Mountain National Park (ROMO), located
in the mountains west of the urban northern Front Range corridor from
July to October 2014. We report on measurements of ozone from two locations in
the park and a suite of volatile organic compounds (VOCs) measured using a
continuous real-time gas chromatography (GC) system and a quadrupole
proton-transfer-reaction mass spectrometer (PRT-MS) at the ROMO Longs Peak (ROMO-LP) air quality
site. We also measured VOCs using canister samples collected along transects
connecting the NFRMA and ROMO. These datasets show that ROMO is impacted by
NFRMA emission sources, and high observed mixing ratios of VOCs associated
with oil and gas extraction (e.g. ethane) and urban sources (e.g. ethene and
C2Cl4) occur during periods of upslope transport. Hourly ozone
mixing ratios exceeded 70 ppb during six events. Two of the six events were
largely associated with VOCs from the oil and gas sector, three high ozone
events were associated with a mixture of VOCs from urban and oil and gas
sources, and one high ozone event was driven by a stratospheric intrusion.
For the high ozone events most associated with emissions from oil and gas
activities, we estimate that VOCs and NOx from sources along
the Front Range contributed ∼20 ppbv of additional ozone.
Funder
National Park Service
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference73 articles.
1. Abeleira, A., Pollack, I. B., Sive, B., Zhou, Y., Fischer, E. V., and Farmer,
D. K.: Source characterization of volatile organic compounds in the Colorado
Northern Front Range Metropolitan Area during spring and summer 2015, J.
Geophys. Res.-Atmos., 122, 3595–3613, https://doi.org/10.1002/2016JD026227, 2017. 2. Abeleira, A., Sive, B., Swarthout, R. F., Fischer, E. V., Zhou, Y., and
Farmer, D. K.: Seasonality, sources and sinks of C1–C5
alkyl nitrates in the Colorado Front Range, Elem. Sci. Anth., 6, 45–63,
https://doi.org/10.1525/elementa.299, 2018. 3. Ashbaugh, L. L., Malm, W. C., and Sadeh, W. Z.: A residence time probability
analysis of sulfur concentrations at Grand Canyon National Park, Atmos.
Environ., 19, 1263–1270, https://doi.org/10.1016/0004-6981(85)90256-2, 1985. 4. ASTM Standard D1835-16: Standard Specification for Liquefied Petroleum (LP)
Gases, ASTM International, West Conshohocken, PA, available at:
http://www.astm.org (last access: 17 July 2018), 2016. 5. Atkinson, R.: Kinetics and mechanisms of the gas-phase reactions of the
hydroxyl radical with organic compounds under atmospheric conditions, Chem.
Rev., 86, 69–201, https://doi.org/10.1021/cr00071a004, 1986.
Cited by
29 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|