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O3, CH4, CO2, CO, NO2 and NMHC aircraft measurements in the Uinta Basin oil and gas region under low and high ozone conditions in winter 2012 and 2013

Bibliographic Data

ID19568397
AuthorsS J Oltmans (0000-0002-7390-2553, Cooperative Institute for Research in Environmental Sciences), A Karion (0000-0002-6304-3513, National Institute of Standards and Technology), R C Schnell (0000-0002-5792-6205, NOAA Earth System Research Laboratory), Gabrielle Pétron (0000-0002-7458-5852, Cooperative Institute for Research in Environmental Sciences), Detlev Helmig (0000-0003-1612-1651, Institute of Arctic and Alpine Research), Stephen A Montzka (0000-0002-9396-0400), S Wolter (Cooperative Institute for Research in Environmental Sciences), D Neff, D H Neff (Cooperative Institute for Research in Environmental Sciences), B R Miller (0000-0002-6686-6849, Cooperative Institute for Research in Environmental Sciences), Jacques Hueber (Institute of Arctic and Alpine Research), Stephen Conley (0000-0001-6753-8962, Scientific Aviation (United States)), B J JOHNSON (0000-0002-7268-9957, NOAA Earth System Research Laboratory), Colm Sweeney (0000-0002-4517-0797, Cooperative Institute for Research in Environmental Sciences)
EditorsMichael E Chang (0000-0001-7226-9736), Brian Lamb (0000-0001-7641-5227)
Year2016
Volume4
Publication date2016-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.12952/journal.elementa.000132
OpenAlexW2542000086
LanguageEN
Citations received4
References cited27

Instrumented aircraft measuring air composition in the Uinta Basin, Utah, during February 2012 and January-February 2013 documented dramatically different atmospheric ozone (O3) mole fractions. In 2012 O3 remained near levels of ∼40 ppb in a well-mixed 500–1000 m deep boundary layer while in 2013, O3 mole fractions >140 ppb were measured in a shallow (∼200 m) boundary layer. In contrast to 2012 when mole fractions of emissions from oil and gas production such as methane (CH4), non-methane hydrocarbons (NMHCs) and combustion products such as carbon dioxide (CO2) were moderately elevated, in winter 2013 very high mole fractions were observed. Snow cover in 2013 helped produce and maintain strong temperature inversions that capped a shallow cold pool layer. In 2012, O3 and CH4 and associated NMHCs mole fractions were not closely related. In 2013, O3 mole fractions were correlated with CH4 and a suite of NMHCs identifying the gas field as the primary source of the O3 precursor NMHC emissions. In 2013 there was a strong positive correlation between CH4 and CO2 suggesting combustion from oil and natural gas processing activities. The presence of O3 precursor NMHCs through the depth of the boundary layer in 2013 led to O3 production throughout the layer. In 2013, O3 mole fractions increased over the course of the week-long episodes indicating O3 photochemical production was larger than dilution and deposition rates, while CH4 mole fractions began to level off after 3 days indicative of some air being mixed out of the boundary layer. The plume of a coal-fired power plant located east of the main gas field was not an important contributor to O3 or O3 precursors in the boundary layer in 2013

Atmospheric sciences · Carbon dioxide · Combustion · Dilution · Methane · Mole fraction · Ozone · Physics · Atmospheric and Environmental Gas Dynamics · Atmospheric chemistry and aerosols · Atmospheric Ozone and Climate · Chemistry · Environmental Science · Geology · Organic Chemistry

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Unique citing works4
Citations per year0,44
Citation span2017 - 2020 (4)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 3

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