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• W2586776887 abstract "High ozone (O3) concentrations at low altitudes (1.5–4 km) were detected from airborne Alpha Jet Atmospheric eXperiment (AJAX) measurements on 30 May 2012 off the coast of California (CA). We investigate the causes of those elevated O3 concentrations using airborne measurements and various models. GEOS-Chem simulation shows that the contribution from local sources is likely small. A back-trajectory model was used to determine the air mass origins and how much they contributed to the O3 over CA. Low-level potential vorticity (PV) from Modern Era Retrospective analysis for Research and Applications 2 (MERRA-2) reanalysis data appears to be a result of the diabatic heating and mixing of airs in the lower altitudes, rather than be a result of direct transport from stratospheric intrusion. The Q diagnostic, which is a measure of the mixing of the air masses, indicates that there is sufficient mixing along the trajectory to indicate that O3 from the different origins is mixed and transported to the western U.S. The back-trajectory model simulation demonstrates the air masses of interest came mostly from the mid troposphere (MT, 76%), but the contribution of the lower troposphere (LT, 19%) is also significant compared to those from the upper troposphere/lower stratosphere (UT/LS, 5%). Air coming from the LT appears to be mostly originating over Asia. The possible surface impact of the high O3 transported aloft on the surface O3 concentration through vertical and horizontal transport within a few days is substantiated by the influence maps determined from the Weather Research and Forecasting–Stochastic Time Inverted Lagrangian Transport (WRF-STILT) model and the observed increases in surface ozone mixing ratios. Contrasting this complex case with a stratospheric-dominant event emphasizes the contribution of each source to the high O3 concentration in the lower altitudes over CA. Integrated analyses using models, reanalysis, and diagnostic tools, allows high ozone values detected by in-situ measurements to be attributed to multiple source processes." @default.
• W2586776887 created "2017-02-17" @default.
• W2586776887 creator A5033784639 @default.
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• W2586776887 date "2017-04-01" @default.
• W2586776887 modified "2023-09-24" @default.
• W2586776887 title "Investigating sources of ozone over California using AJAX airborne measurements and models: Assessing the contribution from long-range transport" @default.
• W2586776887 cites W1509529218 @default.
• W2586776887 cites W1550981726 @default.
• W2586776887 cites W1604414282 @default.
• W2586776887 cites W1627199030 @default.
• W2586776887 cites W1833367443 @default.
• W2586776887 cites W1856745631 @default.
• W2586776887 cites W1904230536 @default.
• W2586776887 cites W1966132318 @default.
• W2586776887 cites W1970536305 @default.
• W2586776887 cites W1972358138 @default.
• W2586776887 cites W1975871748 @default.
• W2586776887 cites W1976498622 @default.
• W2586776887 cites W1978477930 @default.
• W2586776887 cites W1978674556 @default.
• W2586776887 cites W1982322523 @default.
• W2586776887 cites W1985794946 @default.
• W2586776887 cites W1993076417 @default.
• W2586776887 cites W2002316323 @default.
• W2586776887 cites W2009835605 @default.
• W2586776887 cites W2012086419 @default.
• W2586776887 cites W2012805060 @default.
• W2586776887 cites W2021350270 @default.
• W2586776887 cites W2025259712 @default.
• W2586776887 cites W2026659560 @default.
• W2586776887 cites W2029017698 @default.
• W2586776887 cites W2029211844 @default.
• W2586776887 cites W2030195284 @default.
• W2586776887 cites W2046666998 @default.
• W2586776887 cites W2068496264 @default.
• W2586776887 cites W2069348069 @default.
• W2586776887 cites W2070394132 @default.
• W2586776887 cites W2070533532 @default.
• W2586776887 cites W2070977713 @default.
• W2586776887 cites W2076158447 @default.
• W2586776887 cites W2078757038 @default.
• W2586776887 cites W2086378400 @default.
• W2586776887 cites W2087662098 @default.
• W2586776887 cites W2088227539 @default.
• W2586776887 cites W2099255394 @default.
• W2586776887 cites W2100121820 @default.
• W2586776887 cites W2101462621 @default.
• W2586776887 cites W2104718076 @default.
• W2586776887 cites W2105103805 @default.
• W2586776887 cites W2106028503 @default.
• W2586776887 cites W2108896901 @default.
• W2586776887 cites W2115302477 @default.
• W2586776887 cites W2117213541 @default.
• W2586776887 cites W2134856288 @default.
• W2586776887 cites W2134927874 @default.
• W2586776887 cites W2136785010 @default.
• W2586776887 cites W2138017294 @default.
• W2586776887 cites W2138760920 @default.
• W2586776887 cites W2140805694 @default.
• W2586776887 cites W2141510474 @default.
• W2586776887 cites W2143670244 @default.
• W2586776887 cites W2146512399 @default.
• W2586776887 cites W2153712207 @default.
• W2586776887 cites W2154710695 @default.
• W2586776887 cites W2155829461 @default.
• W2586776887 cites W2157486648 @default.
• W2586776887 cites W2159639772 @default.
• W2586776887 cites W2161621332 @default.
• W2586776887 cites W2163464065 @default.
• W2586776887 cites W2165708514 @default.
• W2586776887 cites W2166192216 @default.
• W2586776887 cites W2166607127 @default.
• W2586776887 cites W2168054901 @default.
• W2586776887 cites W2169101778 @default.
• W2586776887 cites W2170222626 @default.
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• W2586776887 cites W2173251738 @default.
• W2586776887 cites W2176254346 @default.
• W2586776887 cites W2609916961 @default.
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• W2586776887 doi "https://doi.org/10.1016/j.atmosenv.2017.02.008" @default.
• W2586776887 hasPublicationYear "2017" @default.
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