2016
DOI: 10.5194/acp-16-6537-2016
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Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East

Abstract: Abstract. Significant progress has been made in identifying the influence of different processes and emissions on the summertime enhancements of free tropospheric ozone (O 3 ) at northern midlatitude regions. However, the exact contribution of regional emissions, chemical and transport processes to these summertime enhancements is still not well quantified. Here we focus on quantifying the influence of regional emissions on the summertime O 3 enhancements over the Middle East, using updated reactive nitrogen (… Show more

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Cited by 12 publications
(10 citation statements)
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“…For retrieval of O 3 from remote sensing measurements, the a priori knowledge is usually taken from an O 3 profile climatology, which provides average O 3 profiles and their variances. Most, if not all, total O 3 algorithms (e.g., Mateer et al, 1971;Klenk et al, 1982;Bhartia and Wellemeyer, 2002;Coldewey-Egbers et al, 2005;Eskes et al, 2005;Veefkind et al, 2006;Lerot et al, 2010Lerot et al, , 2014Loyola et al, 2011;Van Roozendael et al, 2006Wassmann et al, 2015) rely on an O 3 profile climatology to uniquely and completely specify the vertical distribution of a retrieved total column. Profile O 3 algorithms (e.g., Hoogen et al, 1999;Liu et al, 2005;Wei et al, 2010;Bhartia et al, 2013;Miles et al, 2015) based on the widely adopted optimal estimation (OE) inversion technique (Rodgers, 2000) require the a priori O 3 profiles and their covariances to constrain the retrievals from deviating too far from the a priori O 3 distributions.…”
Section: Profile Climatologymentioning
confidence: 99%
“…For retrieval of O 3 from remote sensing measurements, the a priori knowledge is usually taken from an O 3 profile climatology, which provides average O 3 profiles and their variances. Most, if not all, total O 3 algorithms (e.g., Mateer et al, 1971;Klenk et al, 1982;Bhartia and Wellemeyer, 2002;Coldewey-Egbers et al, 2005;Eskes et al, 2005;Veefkind et al, 2006;Lerot et al, 2010Lerot et al, , 2014Loyola et al, 2011;Van Roozendael et al, 2006Wassmann et al, 2015) rely on an O 3 profile climatology to uniquely and completely specify the vertical distribution of a retrieved total column. Profile O 3 algorithms (e.g., Hoogen et al, 1999;Liu et al, 2005;Wei et al, 2010;Bhartia et al, 2013;Miles et al, 2015) based on the widely adopted optimal estimation (OE) inversion technique (Rodgers, 2000) require the a priori O 3 profiles and their covariances to constrain the retrievals from deviating too far from the a priori O 3 distributions.…”
Section: Profile Climatologymentioning
confidence: 99%
“…The seven sites are chosen to represent two longitudinal and 3-4 latitudinal zones in Africa. The meteorological data include the NCEP/NCAR reanalysis I (Kalnay et al, 1996). The monthly wind fields are used to describe the climatology of atmospheric circulation during the study period from 1987 to 2006.…”
Section: The Hysplit Trajectory Model and Meteorological Datamentioning
confidence: 99%
“…Surface O 3 is produced in the atmosphere via photochemical processing of multiple precursors including volatile organic compounds (VOCs), carbon monoxide (CO) and nitrogen oxides (NO,NO 2 ). These precursors originate from both natural and anthropogenic sources (Vingarzan, 2004;Simon et al, 2014;Jiang et al, 2016). In addition to local production, transport of O 3 and its precursors from upwind regions and the upper atmosphere can also influence surface O 3 abundance.…”
Section: Introductionmentioning
confidence: 99%
“…Increases in solar radiation and air temperature can increase the rate of the chemical production of O 3 and modulate the biogenic emissions of O 3 precursors (Guenther, 1993;Sillman and Samson, 1995;Peñuelas and Llusià, 2001), especially over highly polluted regions (Ordónez et al, 2005;Rasmussen et al, 2012;Pusede et al, 2015). Increases in humidity can enhance the chemical destruction of O 3 and shorten its atmospheric lifetime (Johnson et al, 1999;Camalier et al, 2007). Therefore, changes in meteorological conditions on various spatial and temporal scales play key roles in determining the surface O 3 distribution.…”
Section: Introductionmentioning
confidence: 99%