title: Increasing springtime ozone mixing ratios in the free troposphere over western North America.
abstract: In the lowermost layer of the atmosphere-the troposphere-ozone is an important source of the hydroxyl radical, an oxidant that breaks down most pollutants and some greenhouse gases. High concentrations of tropospheric ozone are toxic, however, and have a detrimental effect on human health and ecosystem productivity. Moreover, tropospheric ozone itself acts as an effective greenhouse gas. Much of the present tropospheric ozone burden is a consequence of anthropogenic emissions of ozone precursors resulting in widespread increases in ozone concentrations since the late 1800s. At present, east Asia has the fastest-growing ozone precursor emissions. Much of the springtime east Asian pollution is exported eastwards towards western North America. Despite evidence that the exported Asian pollution produces ozone, no previous study has found a significant increase in free tropospheric ozone concentrations above the western USA since measurements began in the late 1970s. Here we compile springtime ozone measurements from many different platforms across western North America. We show a strong increase in springtime ozone mixing ratios during 1995-2008 and we have some additional evidence that a similar rate of increase in ozone mixing ratio has occurred since 1984. We find that the rate of increase in ozone mixing ratio is greatest when measurements are more heavily influenced by direct transport from Asia. Our result agrees with previous modelling studies, which indicate that global ozone concentrations should be increasing during the early part of the twenty-first century as a result of increasing precursor emissions, especially at northern mid-latitudes, with western North America being particularly sensitive to rising Asian emissions. We suggest that the observed increase in springtime background ozone mixing ratio may hinder the USA's compliance with its ozone air quality standard.
authors.affiliation: Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, USA. owen.r.cooper@noaa.gov
authors.forename: O R
authors.initials: OR
authors.lastname: Cooper
authors.forename: D D
authors.initials: DD
authors.lastname: Parrish
authors.forename: A
authors.initials: A
authors.lastname: Stohl
authors.forename: M
authors.initials: M
authors.lastname: Trainer
authors.forename: P
authors.initials: P
authors.lastname: Nédélec
authors.forename: V
authors.initials: V
authors.lastname: Thouret
authors.forename: J P
authors.initials: JP
authors.lastname: Cammas
authors.forename: S J
authors.initials: SJ
authors.lastname: Oltmans
authors.forename: B J
authors.initials: BJ
authors.lastname: Johnson
authors.forename: D
authors.initials: D
authors.lastname: Tarasick
authors.forename: T
authors.initials: T
authors.lastname: Leblanc
authors.forename: I S
authors.initials: IS
authors.lastname: McDermid
authors.forename: D
authors.initials: D
authors.lastname: Jaffe
authors.forename: R
authors.initials: R
authors.lastname: Gao
authors.forename: J
authors.initials: J
authors.lastname: Stith
authors.forename: T
authors.initials: T
authors.lastname: Ryerson
authors.forename: K
authors.initials: K
authors.lastname: Aikin
authors.forename: T
authors.initials: T
authors.lastname: Campos
authors.forename: A
authors.initials: A
authors.lastname: Weinheimer
authors.forename: M A
authors.initials: MA
authors.lastname: Avery
mesh_terms: D000393:Air Pollutants / Q000032:analysis / Q000737:chemistry; D001208:Asia; D001272:Atmosphere / Q000737:chemistry*; D017753:Ecosystem; D017752:Greenhouse Effect; D049673:History, 20th Century; D049674:History, 21st Century; D009656:North America; D010126:Ozone / Q000032:analysis* / Q000138:chemical synthesis / Q000737:chemistry; D018401:Sample Size; D012621:Seasons
chemical_list: D000393:Air Pollutants; D010126:Ozone