Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4

International audience Anthropogenic pollution and wildfires are main producers of carbon monoxide (CO) and black carbon (BC) in the Northern Hemisphere. High concentrations of these compounds are transported into the Arctic troposphere, influencing the ecosystem in high northern latitudes and the g...

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Main Authors: Tilmes, S., Emmons, L. K., Law, Kathy S., Ancellet, Gérard, Schlager, H., Paris, J.-D., Fuelberg, Henry E., Streets, D. G., Wiedinmyer, C., Diskin, G. S., Kondo, Y., Holloway, J., Schwarz, J. P., Spackman, J. R., Campos, T., Nédélec, P., Panchenko, M. V.
Other Authors: National Center for Atmospheric Research Boulder (NCAR), TROPO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), 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)-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), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), ICOS-RAMCES (ICOS-RAMCES), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU, Florida State University Tallahassee (FSU), Argonne National Laboratory Lemont (ANL), NASA Langley Research Center Hampton (LaRC), Research Center for Advanced Science and Technology Tokyo (RCAST), The University of Tokyo (UTokyo), NOAA Earth System Research Laboratory (ESRL), National Oceanic and Atmospheric Administration (NOAA), Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA), Laboratoire d'aérologie (LAERO), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), V.E. Zuev Institute of Atmospheric Optics (IAO), Siberian Branch of the Russian Academy of Sciences (SB RAS)
Format: Report
Language:English
Published: HAL CCSD 2015
Subjects:
Online Access:https://hal.science/hal-00568788
https://hal.science/hal-00568788/document
https://hal.science/hal-00568788/file/acpd-11-5935-2011.pdf
https://doi.org/10.5194/acpd-11-5935-2011
id ftunivnantes:oai:HAL:hal-00568788v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDE.ES]Environmental Sciences/Environmental and Society
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle [SDE.ES]Environmental Sciences/Environmental and Society
[SDE.MCG]Environmental Sciences/Global Changes
Tilmes, S.
Emmons, L. K.
Law, Kathy S.
Ancellet, Gérard
Schlager, H.
Paris, J.-D.
Fuelberg, Henry E.
Streets, D. G.
Wiedinmyer, C.
Diskin, G. S.
Kondo, Y.
Holloway, J.
Schwarz, J. P.
Spackman, J. R.
Campos, T.
Nédélec, P.
Panchenko, M. V.
Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
topic_facet [SDE.ES]Environmental Sciences/Environmental and Society
[SDE.MCG]Environmental Sciences/Global Changes
description International audience Anthropogenic pollution and wildfires are main producers of carbon monoxide (CO) and black carbon (BC) in the Northern Hemisphere. High concentrations of these compounds are transported into the Arctic troposphere, influencing the ecosystem in high northern latitudes and the global climate. The global chemical transport model MOZART-4 is used to quantify the seasonal evolution of the contribution of CO and BC from different source regions in spring and summer 2008 by tagging their emissions. Aircraft observations from the POLARCAT experiments, in particular NASA ARCTAS, NOAA ARCPAC, POLARCAT-France, DLR GRACE and YAK-AEROSIB, as well as the NSF START08/preHIPPO experiments during Spring-Summer 2008 are combined to quantify the representation of simulated tracer characteristics in anthropogenic and fire plumes. In general, the model reproduces CO and BC well. Based on aircraft measurements and FLEXPART back-trajectories, the altitude contribution of emissions coming from different source regions is well captured in the model. Uncertainties of the MOZART-4 model are identified by comparing the data with model results on the flight tracks and using MOPITT satellite observations. Anthropogenic emissions are underestimated by about 10% in high northern latitudes in spring, and shortcomings exist in simulating fire plumes. The remote impact of East-Siberian fire emissions is underestimated for spring, whereas the impact of Southeast Asian fire emissions to mid-latitude CO values is overestimated by the model. In summer, mid-latitude CO values agree well between model and observations, whereas summer high latitude East-Siberian fire emissions in the model are overestimated by 20% in comparison to observations in the region. On the other hand, CO concentrations are underestimated by about 30% over Alaska and Canada at altitudes above 4 km. BC values are overestimated by the model at altitudes above 4 km in summer. Based on MOZART-4, with tagged CO and BC tracers, anthropogenic emissions of Asia, ...
author2 National Center for Atmospheric Research Boulder (NCAR)
TROPO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
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)-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)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
ICOS-RAMCES (ICOS-RAMCES)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU
Florida State University Tallahassee (FSU)
Argonne National Laboratory Lemont (ANL)
NASA Langley Research Center Hampton (LaRC)
Research Center for Advanced Science and Technology Tokyo (RCAST)
The University of Tokyo (UTokyo)
NOAA Earth System Research Laboratory (ESRL)
National Oceanic and Atmospheric Administration (NOAA)
Cooperative Institute for Research in Environmental Sciences (CIRES)
University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA)
Laboratoire d'aérologie (LAERO)
Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)
V.E. Zuev Institute of Atmospheric Optics (IAO)
Siberian Branch of the Russian Academy of Sciences (SB RAS)
format Report
author Tilmes, S.
Emmons, L. K.
Law, Kathy S.
Ancellet, Gérard
Schlager, H.
Paris, J.-D.
Fuelberg, Henry E.
Streets, D. G.
Wiedinmyer, C.
Diskin, G. S.
Kondo, Y.
Holloway, J.
Schwarz, J. P.
Spackman, J. R.
Campos, T.
Nédélec, P.
Panchenko, M. V.
author_facet Tilmes, S.
Emmons, L. K.
Law, Kathy S.
Ancellet, Gérard
Schlager, H.
Paris, J.-D.
Fuelberg, Henry E.
Streets, D. G.
Wiedinmyer, C.
Diskin, G. S.
Kondo, Y.
Holloway, J.
Schwarz, J. P.
Spackman, J. R.
Campos, T.
Nédélec, P.
Panchenko, M. V.
author_sort Tilmes, S.
title Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
title_short Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
title_full Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
title_fullStr Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
title_full_unstemmed Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4
title_sort source contributions to northern hemisphere co and black carbon during spring and summer 2008 from polarcat and start08/prehippo observations and mozart-4
publisher HAL CCSD
publishDate 2015
url https://hal.science/hal-00568788
https://hal.science/hal-00568788/document
https://hal.science/hal-00568788/file/acpd-11-5935-2011.pdf
https://doi.org/10.5194/acpd-11-5935-2011
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
black carbon
Alaska
genre_facet Arctic
black carbon
Alaska
op_source ISSN: 1680-7367
EISSN: 1680-7375
Atmospheric Chemistry and Physics Discussions
https://hal.science/hal-00568788
2015
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acpd-11-5935-2011
hal-00568788
https://hal.science/hal-00568788
https://hal.science/hal-00568788/document
https://hal.science/hal-00568788/file/acpd-11-5935-2011.pdf
doi:10.5194/acpd-11-5935-2011
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acpd-11-5935-2011
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spelling ftunivnantes:oai:HAL:hal-00568788v1 2023-05-15T15:18:38+02:00 Source contributions to Northern Hemisphere CO and black carbon during spring and summer 2008 from POLARCAT and START08/preHIPPO observations and MOZART-4 Tilmes, S. Emmons, L. K. Law, Kathy S. Ancellet, Gérard Schlager, H. Paris, J.-D. Fuelberg, Henry E. Streets, D. G. Wiedinmyer, C. Diskin, G. S. Kondo, Y. Holloway, J. Schwarz, J. P. Spackman, J. R. Campos, T. Nédélec, P. Panchenko, M. V. National Center for Atmospheric Research Boulder (NCAR) TROPO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) 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)-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) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) ICOS-RAMCES (ICOS-RAMCES) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU Florida State University Tallahassee (FSU) Argonne National Laboratory Lemont (ANL) NASA Langley Research Center Hampton (LaRC) Research Center for Advanced Science and Technology Tokyo (RCAST) The University of Tokyo (UTokyo) NOAA Earth System Research Laboratory (ESRL) National Oceanic and Atmospheric Administration (NOAA) Cooperative Institute for Research in Environmental Sciences (CIRES) University of Colorado Boulder -National Oceanic and Atmospheric Administration (NOAA) Laboratoire d'aérologie (LAERO) Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) V.E. Zuev Institute of Atmospheric Optics (IAO) Siberian Branch of the Russian Academy of Sciences (SB RAS) 2015-12-22 https://hal.science/hal-00568788 https://hal.science/hal-00568788/document https://hal.science/hal-00568788/file/acpd-11-5935-2011.pdf https://doi.org/10.5194/acpd-11-5935-2011 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acpd-11-5935-2011 hal-00568788 https://hal.science/hal-00568788 https://hal.science/hal-00568788/document https://hal.science/hal-00568788/file/acpd-11-5935-2011.pdf doi:10.5194/acpd-11-5935-2011 info:eu-repo/semantics/OpenAccess ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.science/hal-00568788 2015 [SDE.ES]Environmental Sciences/Environmental and Society [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/preprint Preprints, Working Papers, . 2015 ftunivnantes https://doi.org/10.5194/acpd-11-5935-2011 2023-02-22T10:33:51Z International audience Anthropogenic pollution and wildfires are main producers of carbon monoxide (CO) and black carbon (BC) in the Northern Hemisphere. High concentrations of these compounds are transported into the Arctic troposphere, influencing the ecosystem in high northern latitudes and the global climate. The global chemical transport model MOZART-4 is used to quantify the seasonal evolution of the contribution of CO and BC from different source regions in spring and summer 2008 by tagging their emissions. Aircraft observations from the POLARCAT experiments, in particular NASA ARCTAS, NOAA ARCPAC, POLARCAT-France, DLR GRACE and YAK-AEROSIB, as well as the NSF START08/preHIPPO experiments during Spring-Summer 2008 are combined to quantify the representation of simulated tracer characteristics in anthropogenic and fire plumes. In general, the model reproduces CO and BC well. Based on aircraft measurements and FLEXPART back-trajectories, the altitude contribution of emissions coming from different source regions is well captured in the model. Uncertainties of the MOZART-4 model are identified by comparing the data with model results on the flight tracks and using MOPITT satellite observations. Anthropogenic emissions are underestimated by about 10% in high northern latitudes in spring, and shortcomings exist in simulating fire plumes. The remote impact of East-Siberian fire emissions is underestimated for spring, whereas the impact of Southeast Asian fire emissions to mid-latitude CO values is overestimated by the model. In summer, mid-latitude CO values agree well between model and observations, whereas summer high latitude East-Siberian fire emissions in the model are overestimated by 20% in comparison to observations in the region. On the other hand, CO concentrations are underestimated by about 30% over Alaska and Canada at altitudes above 4 km. BC values are overestimated by the model at altitudes above 4 km in summer. Based on MOZART-4, with tagged CO and BC tracers, anthropogenic emissions of Asia, ... Report Arctic black carbon Alaska Université de Nantes: HAL-UNIV-NANTES Arctic Canada