Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign

Abstract. A case of continental outflow from the United States (US) was examined using airborne measurements from NASA DC-8 flight 13 during the Intercontinental Chemical Transport Experiment -North America (INTEX-NA). Mixing ratios of methane (CH 4 ) and carbon monoxide (CO) at 8-11 km altitude ove...

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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1035.8657 2023-05-15T17:27:50+02:00 Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign The Pennsylvania State University CiteSeerX Archives http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1035.8657 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1035.8657 Metadata may be used without restrictions as long as the oai identifier remains attached to it. text ftciteseerx 2020-02-16T01:15:39Z Abstract. A case of continental outflow from the United States (US) was examined using airborne measurements from NASA DC-8 flight 13 during the Intercontinental Chemical Transport Experiment -North America (INTEX-NA). Mixing ratios of methane (CH 4 ) and carbon monoxide (CO) at 8-11 km altitude over the North Atlantic were elevated to 1843 ppbv and 134 ppbv respectively, while those of carbon dioxide (CO 2 ) and carbonyl sulfide (COS) were reduced to 372.4 ppmv and 411 pptv respectively. In this region, urban and industrial influences were evidenced by elevated mixing ratios and good linear relationships between urban and industrial tracers compared to North Atlantic background air. Moreover, low mixing ratios and a good correlation between COS and CO 2 showed a fingerprint of terrestrial uptake and minimal dilution during rapid transport over a 1-2 day time period. Analysis of synoptic conditions, backward trajectories, and photochemical aging estimates based on C 3 H 8 /C 2 H 6 strongly suggested that elevated anthropogenic tracers in the upper troposphere of the flight region were the result of transport via convection and warm conveyor belt (WCB) uplifting of boundary layer air over the southeastern US. This mechanism is supported by the similar slope values of linear correlations between long-lived (months) anthropogenic tracers (e.g., C 2 Cl 4 and CHCl 3 ) from the flight region and the planetary boundary layer in the southeastern US. In addition, the aircraft measurements suggest that outflow from the US augmented the entire tropospheric column at mid-latitudes over the North Atlantic. Overall, the flight 13 data demonstrate a pervasive impact of US anthropogenic emissions on the troposphere over the North Atlantic. Text North Atlantic Unknown
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description Abstract. A case of continental outflow from the United States (US) was examined using airborne measurements from NASA DC-8 flight 13 during the Intercontinental Chemical Transport Experiment -North America (INTEX-NA). Mixing ratios of methane (CH 4 ) and carbon monoxide (CO) at 8-11 km altitude over the North Atlantic were elevated to 1843 ppbv and 134 ppbv respectively, while those of carbon dioxide (CO 2 ) and carbonyl sulfide (COS) were reduced to 372.4 ppmv and 411 pptv respectively. In this region, urban and industrial influences were evidenced by elevated mixing ratios and good linear relationships between urban and industrial tracers compared to North Atlantic background air. Moreover, low mixing ratios and a good correlation between COS and CO 2 showed a fingerprint of terrestrial uptake and minimal dilution during rapid transport over a 1-2 day time period. Analysis of synoptic conditions, backward trajectories, and photochemical aging estimates based on C 3 H 8 /C 2 H 6 strongly suggested that elevated anthropogenic tracers in the upper troposphere of the flight region were the result of transport via convection and warm conveyor belt (WCB) uplifting of boundary layer air over the southeastern US. This mechanism is supported by the similar slope values of linear correlations between long-lived (months) anthropogenic tracers (e.g., C 2 Cl 4 and CHCl 3 ) from the flight region and the planetary boundary layer in the southeastern US. In addition, the aircraft measurements suggest that outflow from the US augmented the entire tropospheric column at mid-latitudes over the North Atlantic. Overall, the flight 13 data demonstrate a pervasive impact of US anthropogenic emissions on the troposphere over the North Atlantic.
author2 The Pennsylvania State University CiteSeerX Archives
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title Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
spellingShingle Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
title_short Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
title_full Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
title_fullStr Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
title_full_unstemmed Continental outflow from the US to the upper troposphere over the North Atlantic during the NASA INTEX-NA Airborne Campaign
title_sort continental outflow from the us to the upper troposphere over the north atlantic during the nasa intex-na airborne campaign
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1035.8657
genre North Atlantic
genre_facet North Atlantic
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