Atmospheric chemical transport based on high-resolution model-derived winds: A case study

Flight 10 of NASA's Subsonic Assessment (SASS) Ozone and Nitrogen Oxide Experiment (SONEX) extended southwest of Lajes, Azores. A variety of chemical signatures was encountered. These signatures are examined in detail, relating them to meteorological data from a high‐resolution numerical model...

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Veröffentlicht in:Journal of Geophysical Research, Washington, DC Washington, DC, 2000-02, Vol.105 (D3), p.3807-3820
Hauptverfasser: Hannan, John R., Fuelberg, Henry E., Thompson, Anne M., Bieberbach, George, Knabb, Richard D., Kondo, Yutaka, Anderson, Bruce E., Browell, Edward V., Gregory, Gerald L., Sachse, Glen W., Singh, Hanwant B.
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Sprache:eng
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Zusammenfassung:Flight 10 of NASA's Subsonic Assessment (SASS) Ozone and Nitrogen Oxide Experiment (SONEX) extended southwest of Lajes, Azores. A variety of chemical signatures was encountered. These signatures are examined in detail, relating them to meteorological data from a high‐resolution numerical model having a horizontal grid spacing of 30 and 90 km with 26 vertical levels. The meteorological output at hourly intervals is used to create backward trajectories from the locations of the chemical signatures. Four major categories of chemical signatures are discussed: stratospheric, lightning, continental pollution, and a mixed chemical layer. The strong stratospheric signal is encountered just south of the Azores in a region of depressed tropopause height. Three chemical signatures at different altitudes in the upper troposphere are attributed to lightning. Backward trajectories from these signatures extend to locations of cloud‐to‐ground lightning. Specifically, results show that the trajectories pass over regions of lightning 1–2 days earlier over the eastern Gulf of Mexico and off the southeast coast of the United States. The lowest leg of the flight exhibits a chemical signature consistent with continental pollution. Trajectories from this signature are found to pass over the highly populated Northeast Corridor of the United States. Surface‐based pollution apparently is lofted to the altitudes of the trajectories by convective clouds along the East Coast that did not contain lightning. Finally, a mixed layer is described. Its chemical signature is intermediate to those of lightning and continental pollution. Backward trajectories from this layer pass between the trajectories of the lightning and pollution signatures. Thus they likely are impacted by both sources.
ISSN:0148-0227
2156-2202
DOI:10.1029/1999JD900989