Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic

A case of long-range transport of a biomass burning plume from Alaska to Europe is analyzed using a Lagrangian approach. This plume was sampled several times in the free troposphere over North America, the North Atlantic and Europe by three different aircraft during the IGAC Lagrangian 2K4 experimen...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Real, Elsa, Law, Kathy S., Weinzierl, Bernadett, Fiebig, M., Petzold, A., Wild, O., Methven, J., Arnold, S., Stohl, A., Huntrieser, H., Roiger, Anke, Schlager, H., Stewart, D., Avery, M., Sachse, G., Browell, E., Ferrare, R., Blake, D.
Other Authors: Service d'aéronomie (SA), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), DLR Institut für Physik der Atmosphäre (IPA), Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR), Centre for Atmospheric Science Cambridge, UK, University of Cambridge UK (CAM), Department of Meteorology Reading, University of Reading (UOR), School of Earth and Environment Leeds (SEE), University of Leeds, Norwegian Institute for Air Research (NILU), School of Environmental Sciences Norwich, University of East Anglia Norwich (UEA), NASA Langley Research Center Hampton (LaRC), Department of Chemistry Irvine, University of California Irvine (UCI), University of California-University of California, INSU-CNRS, ADEME, Institut Pierre Simon Laplace (IPSL), Institut Geographique National (IGN)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-00164294
https://hal.archives-ouvertes.fr/hal-00164294/document
https://hal.archives-ouvertes.fr/hal-00164294/file/Real_et_al-2007-Journal_of_Geophysical_Research__Atmospheres_%281984-2012%29.pdf
https://doi.org/10.1029/2006JD007576
id ftccsdartic:oai:HAL:hal-00164294v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic photochemistry
long-range transport
boreal fires
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle photochemistry
long-range transport
boreal fires
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Real, Elsa
Law, Kathy S.
Weinzierl, Bernadett
Fiebig, M.
Petzold, A.
Wild, O.
Methven, J.
Arnold, S.
Stohl, A.
Huntrieser, H.
Roiger, Anke
Schlager, H.
Stewart, D.
Avery, M.
Sachse, G.
Browell, E.
Ferrare, R.
Blake, D.
Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
topic_facet photochemistry
long-range transport
boreal fires
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description A case of long-range transport of a biomass burning plume from Alaska to Europe is analyzed using a Lagrangian approach. This plume was sampled several times in the free troposphere over North America, the North Atlantic and Europe by three different aircraft during the IGAC Lagrangian 2K4 experiment which was part of the ICARTT/ITOP measurement intensive in summer 2004. Measurements in the plume showed enhanced values of CO, VOCs and NO y , mainly in form of PAN. Observed O 3 levels increased by 17 ppbv over 5 days. A photochemical trajectory model, CiTTyCAT, was used to examine processes responsible for the chemical evolution of the plume. The model was initialized with upwind data and compared with downwind measurements. The influence of high aerosol loading on photolysis rates in the plume was investigated using in situ aerosol measurements in the plume and lidar retrievals of optical depth as input into a photolysis code (Fast-J), run in the model. Significant impacts on photochemistry are found with a decrease of 18% in O 3 production and 24% in O 3 destruction over 5 days when including aerosols. The plume is found to be chemically active with large O 3 increases attributed primarily to PAN decomposition during descent of the plume toward Europe. The predicted O 3 changes are very dependent on temperature changes during transport and also on water vapor levels in the lower troposphere which can lead to O 3 destruction. Simulation of mixing/dilution was necessary to reproduce observed pollutant levels in the plume. Mixing was simulated using background concentrations from measurements in air masses in close proximity to the plume, and mixing timescales (averaging 6.25 days) were derived from CO changes. Observed and simulated O 3 /CO correlations in the plume were also compared in order to evaluate the photochemistry in the model. Observed slopes change from negative to positive over 5 days. This change, which can be attributed largely to photochemistry, is well reproduced by multiple model runs even if ...
author2 Service d'aéronomie (SA)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
DLR Institut für Physik der Atmosphäre (IPA)
Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR)
Centre for Atmospheric Science Cambridge, UK
University of Cambridge UK (CAM)
Department of Meteorology Reading
University of Reading (UOR)
School of Earth and Environment Leeds (SEE)
University of Leeds
Norwegian Institute for Air Research (NILU)
School of Environmental Sciences Norwich
University of East Anglia Norwich (UEA)
NASA Langley Research Center Hampton (LaRC)
Department of Chemistry Irvine
University of California Irvine (UCI)
University of California-University of California
INSU-CNRS
ADEME
Institut Pierre Simon Laplace (IPSL)
Institut Geographique National (IGN)
format Article in Journal/Newspaper
author Real, Elsa
Law, Kathy S.
Weinzierl, Bernadett
Fiebig, M.
Petzold, A.
Wild, O.
Methven, J.
Arnold, S.
Stohl, A.
Huntrieser, H.
Roiger, Anke
Schlager, H.
Stewart, D.
Avery, M.
Sachse, G.
Browell, E.
Ferrare, R.
Blake, D.
author_facet Real, Elsa
Law, Kathy S.
Weinzierl, Bernadett
Fiebig, M.
Petzold, A.
Wild, O.
Methven, J.
Arnold, S.
Stohl, A.
Huntrieser, H.
Roiger, Anke
Schlager, H.
Stewart, D.
Avery, M.
Sachse, G.
Browell, E.
Ferrare, R.
Blake, D.
author_sort Real, Elsa
title Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
title_short Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
title_full Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
title_fullStr Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
title_full_unstemmed Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic
title_sort processes influencing ozone levels in alaskan forest fire plumes during long-range transport over the north atlantic
publisher HAL CCSD
publishDate 2007
url https://hal.archives-ouvertes.fr/hal-00164294
https://hal.archives-ouvertes.fr/hal-00164294/document
https://hal.archives-ouvertes.fr/hal-00164294/file/Real_et_al-2007-Journal_of_Geophysical_Research__Atmospheres_%281984-2012%29.pdf
https://doi.org/10.1029/2006JD007576
genre North Atlantic
Alaska
genre_facet North Atlantic
Alaska
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://hal.archives-ouvertes.fr/hal-00164294
Journal of Geophysical Research: Atmospheres, American Geophysical Union, 2007, 112, pp.D10S41. ⟨10.1029/2006JD007576⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2006JD007576
hal-00164294
https://hal.archives-ouvertes.fr/hal-00164294
https://hal.archives-ouvertes.fr/hal-00164294/document
https://hal.archives-ouvertes.fr/hal-00164294/file/Real_et_al-2007-Journal_of_Geophysical_Research__Atmospheres_%281984-2012%29.pdf
doi:10.1029/2006JD007576
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2006JD007576
container_title Journal of Geophysical Research: Atmospheres
container_volume 112
container_issue D10
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spelling ftccsdartic:oai:HAL:hal-00164294v1 2023-05-15T17:32:58+02:00 Processes influencing ozone levels in Alaskan forest fire plumes during long-range transport over the North Atlantic Real, Elsa Law, Kathy S. Weinzierl, Bernadett Fiebig, M. Petzold, A. Wild, O. Methven, J. Arnold, S. Stohl, A. Huntrieser, H. Roiger, Anke Schlager, H. Stewart, D. Avery, M. Sachse, G. Browell, E. Ferrare, R. Blake, D. Service d'aéronomie (SA) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) DLR Institut für Physik der Atmosphäre (IPA) Deutsches Zentrum für Luft- und Raumfahrt Oberpfaffenhofen-Wessling (DLR) Centre for Atmospheric Science Cambridge, UK University of Cambridge UK (CAM) Department of Meteorology Reading University of Reading (UOR) School of Earth and Environment Leeds (SEE) University of Leeds Norwegian Institute for Air Research (NILU) School of Environmental Sciences Norwich University of East Anglia Norwich (UEA) NASA Langley Research Center Hampton (LaRC) Department of Chemistry Irvine University of California Irvine (UCI) University of California-University of California INSU-CNRS ADEME Institut Pierre Simon Laplace (IPSL) Institut Geographique National (IGN) 2007 https://hal.archives-ouvertes.fr/hal-00164294 https://hal.archives-ouvertes.fr/hal-00164294/document https://hal.archives-ouvertes.fr/hal-00164294/file/Real_et_al-2007-Journal_of_Geophysical_Research__Atmospheres_%281984-2012%29.pdf https://doi.org/10.1029/2006JD007576 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2006JD007576 hal-00164294 https://hal.archives-ouvertes.fr/hal-00164294 https://hal.archives-ouvertes.fr/hal-00164294/document https://hal.archives-ouvertes.fr/hal-00164294/file/Real_et_al-2007-Journal_of_Geophysical_Research__Atmospheres_%281984-2012%29.pdf doi:10.1029/2006JD007576 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal.archives-ouvertes.fr/hal-00164294 Journal of Geophysical Research: Atmospheres, American Geophysical Union, 2007, 112, pp.D10S41. ⟨10.1029/2006JD007576⟩ photochemistry long-range transport boreal fires [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2007 ftccsdartic https://doi.org/10.1029/2006JD007576 2021-11-21T02:41:15Z A case of long-range transport of a biomass burning plume from Alaska to Europe is analyzed using a Lagrangian approach. This plume was sampled several times in the free troposphere over North America, the North Atlantic and Europe by three different aircraft during the IGAC Lagrangian 2K4 experiment which was part of the ICARTT/ITOP measurement intensive in summer 2004. Measurements in the plume showed enhanced values of CO, VOCs and NO y , mainly in form of PAN. Observed O 3 levels increased by 17 ppbv over 5 days. A photochemical trajectory model, CiTTyCAT, was used to examine processes responsible for the chemical evolution of the plume. The model was initialized with upwind data and compared with downwind measurements. The influence of high aerosol loading on photolysis rates in the plume was investigated using in situ aerosol measurements in the plume and lidar retrievals of optical depth as input into a photolysis code (Fast-J), run in the model. Significant impacts on photochemistry are found with a decrease of 18% in O 3 production and 24% in O 3 destruction over 5 days when including aerosols. The plume is found to be chemically active with large O 3 increases attributed primarily to PAN decomposition during descent of the plume toward Europe. The predicted O 3 changes are very dependent on temperature changes during transport and also on water vapor levels in the lower troposphere which can lead to O 3 destruction. Simulation of mixing/dilution was necessary to reproduce observed pollutant levels in the plume. Mixing was simulated using background concentrations from measurements in air masses in close proximity to the plume, and mixing timescales (averaging 6.25 days) were derived from CO changes. Observed and simulated O 3 /CO correlations in the plume were also compared in order to evaluate the photochemistry in the model. Observed slopes change from negative to positive over 5 days. This change, which can be attributed largely to photochemistry, is well reproduced by multiple model runs even if ... Article in Journal/Newspaper North Atlantic Alaska Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Journal of Geophysical Research: Atmospheres 112 D10