Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East

Significant progress has been made in identifying the influence of different processes and emissions on the summertime enhancements of free tropospheric ozone (O<sub>3</sub>) at northern midlatitude regions. However, the exact contribution of regional emissions, chemical and transport...

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Main Authors: Z. Jiang, K. Miyazaki, J. R. Worden, J. J. Liu, D. B. A. Jones, D. K. Henze
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/6537/2016/acp-16-6537-2016.pdf
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author Z. Jiang
Z. Jiang
K. Miyazaki
J. R. Worden
J. J. Liu
J. J. Liu
D. B. A. Jones
D. K. Henze
author_facet Z. Jiang
Z. Jiang
K. Miyazaki
J. R. Worden
J. J. Liu
J. J. Liu
D. B. A. Jones
D. K. Henze
author_sort Z. Jiang
collection DOAJ
description Significant progress has been made in identifying the influence of different processes and emissions on the summertime enhancements of free tropospheric ozone (O<sub>3</sub>) 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<sub>3</sub> enhancements over the Middle East, using updated reactive nitrogen (NO<sub><i>x</i></sub>) emissions. We then use the adjoint of the GEOS-Chem model with these updated NO<sub><i>x</i></sub> emissions to show that the global total contribution of lightning NO<sub><i>x</i></sub> on middle free tropospheric O<sub>3</sub> over the Middle East is about 2 times larger than that from global anthropogenic sources. The summertime middle free tropospheric O<sub>3</sub> enhancement is primarily due to Asian NO<sub><i>x</i></sub> emissions, with approximately equivalent contributions from Asian anthropogenic activities and lightning. In the Middle Eastern lower free troposphere, lightning NO<sub><i>x</i></sub> from Europe and North America and anthropogenic NO<sub><i>x</i></sub> from Middle Eastern local emissions are the primary sources of O<sub>3</sub>. This work highlights the critical role of lightning NO<sub><i>x</i></sub> on northern midlatitude free tropospheric O<sub>3</sub> and the important effect of the Asian summer monsoon on the export of Asian pollutants.
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spelling doaj.art-a1e6ace4bce14bf3a75a1d3683336d562022-12-21T20:01:18ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-05-01166537654610.5194/acp-16-6537-2016Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle EastZ. Jiang0Z. Jiang1K. Miyazaki2J. R. Worden3J. J. Liu4J. J. Liu5D. B. A. Jones6D. K. Henze7Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USAnow at: National Center for Atmospheric Research, Boulder, CO, USAJapan Agency for Marine-Earth Science and Technology, Yokohama, JapanJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USADepartment of Geography and Planning, University of Toronto, Toronto, ON, CanadaSchool of Atmospheric Sciences, Nanjing University, Nanjing, ChinaDepartment of Physics, University of Toronto, Toronto, ON, CanadaDepartment of Mechanical Engineering, University of Colorado, Boulder, CO, USASignificant progress has been made in identifying the influence of different processes and emissions on the summertime enhancements of free tropospheric ozone (O<sub>3</sub>) 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<sub>3</sub> enhancements over the Middle East, using updated reactive nitrogen (NO<sub><i>x</i></sub>) emissions. We then use the adjoint of the GEOS-Chem model with these updated NO<sub><i>x</i></sub> emissions to show that the global total contribution of lightning NO<sub><i>x</i></sub> on middle free tropospheric O<sub>3</sub> over the Middle East is about 2 times larger than that from global anthropogenic sources. The summertime middle free tropospheric O<sub>3</sub> enhancement is primarily due to Asian NO<sub><i>x</i></sub> emissions, with approximately equivalent contributions from Asian anthropogenic activities and lightning. In the Middle Eastern lower free troposphere, lightning NO<sub><i>x</i></sub> from Europe and North America and anthropogenic NO<sub><i>x</i></sub> from Middle Eastern local emissions are the primary sources of O<sub>3</sub>. This work highlights the critical role of lightning NO<sub><i>x</i></sub> on northern midlatitude free tropospheric O<sub>3</sub> and the important effect of the Asian summer monsoon on the export of Asian pollutants.https://www.atmos-chem-phys.net/16/6537/2016/acp-16-6537-2016.pdf
spellingShingle Z. Jiang
Z. Jiang
K. Miyazaki
J. R. Worden
J. J. Liu
J. J. Liu
D. B. A. Jones
D. K. Henze
Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
Atmospheric Chemistry and Physics
title Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
title_full Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
title_fullStr Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
title_full_unstemmed Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
title_short Impacts of anthropogenic and natural sources on free tropospheric ozone over the Middle East
title_sort impacts of anthropogenic and natural sources on free tropospheric ozone over the middle east
url https://www.atmos-chem-phys.net/16/6537/2016/acp-16-6537-2016.pdf
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