Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions

<p>Ozone is a key constituent of the troposphere, where it drives photochemical processes, impacts air quality, and acts as a climate forcer. Large-scale in situ observations of ozone commensurate with the grid resolution of current Earth system models are necessary to validate model outputs a...

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Main Authors: I. Bourgeois, J. Peischl, C. R. Thompson, K. C. Aikin, T. Campos, H. Clark, R. Commane, B. Daube, G. W. Diskin, J. W. Elkins, R.-S. Gao, A. Gaudel, E. J. Hintsa, B. J. Johnson, R. Kivi, K. McKain, F. L. Moore, D. D. Parrish, R. Querel, E. Ray, R. Sánchez, C. Sweeney, D. W. Tarasick, A. M. Thompson, V. Thouret, J. C. Witte, S. C. Wofsy, T. B. Ryerson
Format: Article
Language:English
Published: Copernicus Publications 2020-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/20/10611/2020/acp-20-10611-2020.pdf
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author I. Bourgeois
I. Bourgeois
J. Peischl
J. Peischl
C. R. Thompson
C. R. Thompson
K. C. Aikin
K. C. Aikin
T. Campos
H. Clark
R. Commane
B. Daube
G. W. Diskin
J. W. Elkins
R.-S. Gao
A. Gaudel
A. Gaudel
E. J. Hintsa
E. J. Hintsa
B. J. Johnson
R. Kivi
K. McKain
K. McKain
F. L. Moore
F. L. Moore
D. D. Parrish
D. D. Parrish
R. Querel
E. Ray
E. Ray
R. Sánchez
C. Sweeney
D. W. Tarasick
A. M. Thompson
V. Thouret
J. C. Witte
S. C. Wofsy
T. B. Ryerson
author_facet I. Bourgeois
I. Bourgeois
J. Peischl
J. Peischl
C. R. Thompson
C. R. Thompson
K. C. Aikin
K. C. Aikin
T. Campos
H. Clark
R. Commane
B. Daube
G. W. Diskin
J. W. Elkins
R.-S. Gao
A. Gaudel
A. Gaudel
E. J. Hintsa
E. J. Hintsa
B. J. Johnson
R. Kivi
K. McKain
K. McKain
F. L. Moore
F. L. Moore
D. D. Parrish
D. D. Parrish
R. Querel
E. Ray
E. Ray
R. Sánchez
C. Sweeney
D. W. Tarasick
A. M. Thompson
V. Thouret
J. C. Witte
S. C. Wofsy
T. B. Ryerson
author_sort I. Bourgeois
collection DOAJ
description <p>Ozone is a key constituent of the troposphere, where it drives photochemical processes, impacts air quality, and acts as a climate forcer. Large-scale in situ observations of ozone commensurate with the grid resolution of current Earth system models are necessary to validate model outputs and satellite retrievals. In this paper, we examine measurements from the Atmospheric Tomography (ATom; four deployments in 2016–2018) and the HIAPER Pole-to-Pole Observations (HIPPO; five deployments in 2009–2011) experiments, two global-scale airborne campaigns covering the Pacific and Atlantic basins.</p> <p>ATom and HIPPO represent the first global-scale, vertically resolved measurements of <span class="inline-formula">O<sub>3</sub></span> distributions throughout the troposphere, with HIPPO sampling the atmosphere over the Pacific and ATom sampling both the Pacific and Atlantic. Given the relatively limited temporal resolution of these two campaigns, we first compare ATom and HIPPO ozone data to longer-term observational records to establish the representativeness of our dataset. We show that these two airborne campaigns captured on average 53&thinsp;%, 54&thinsp;%, and 38&thinsp;% of the ozone variability in the marine boundary layer, free troposphere, and upper troposphere–lower stratosphere (UTLS), respectively, at nine well-established ozonesonde sites. Additionally, ATom captured the most frequent ozone concentrations measured by regular commercial aircraft flights in the northern Atlantic UTLS. We then use the repeated<span id="page10612"/> vertical profiles from these two campaigns to confirm and extend the existing knowledge of tropospheric ozone spatial and vertical distributions throughout the remote troposphere. We highlight a clear hemispheric gradient, with greater ozone in the Northern Hemisphere, consistent with greater precursor emissions and consistent with previous modeling and satellite studies. We also show that the ozone distribution below 8&thinsp;km was similar in the extra-tropics of the Atlantic and Pacific basins, likely due to zonal circulation patterns. However, twice as much ozone was found in the tropical Atlantic as in the tropical Pacific, due to well-documented dynamical patterns transporting continental air masses over the Atlantic. Finally, we show that the seasonal variability of tropospheric ozone over the Pacific and the Atlantic basins is driven year-round by transported continental plumes and photochemistry, and the vertical distribution is driven by photochemistry and mixing with stratospheric air. This new dataset provides additional constraints for global climate and chemistry models to improve our understanding of both ozone production and loss processes in remote regions, as well as the influence of anthropogenic emissions on baseline ozone.</p>
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spelling doaj.art-e8cdef94390d4ddfa0947f719bf68eb62022-12-21T22:41:20ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242020-09-0120106111063510.5194/acp-20-10611-2020Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missionsI. Bourgeois0I. Bourgeois1J. Peischl2J. Peischl3C. R. Thompson4C. R. Thompson5K. C. Aikin6K. C. Aikin7T. Campos8H. Clark9R. Commane10B. Daube11G. W. Diskin12J. W. Elkins13R.-S. Gao14A. Gaudel15A. Gaudel16E. J. Hintsa17E. J. Hintsa18B. J. Johnson19R. Kivi20K. McKain21K. McKain22F. L. Moore23F. L. Moore24D. D. Parrish25D. D. Parrish26R. Querel27E. Ray28E. Ray29R. Sánchez30C. Sweeney31D. W. Tarasick32A. M. Thompson33V. Thouret34J. C. Witte35S. C. Wofsy36T. B. Ryerson37Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USAIAGOS-AISBL, Brussels, BelgiumDepartment of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, New York, NY, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USANASA Langley Research Center, Hampton, VA, USANOAA Global Monitoring Laboratory, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Global Monitoring Laboratory, Boulder, CO, USANOAA Global Monitoring Laboratory, Boulder, CO, USAFinnish Meteorological Institute, Space and Earth Observation Centre, Sodankylä, FinlandCooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Global Monitoring Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Global Monitoring Laboratory, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USANational Institute of Water & Atmospheric Research (NIWA), Lauder, New ZealandCooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USANOAA Chemical Science Laboratory, Boulder, CO, USAServicio Meteorológico Nacional, Buenos Aires, ArgentinaNOAA Global Monitoring Laboratory, Boulder, CO, USAExperimental Studies Research Division, MSC/Environment and Climate Change Canada, Downsview, Ontario, CanadaEarth Sciences Division, NASA Goddard Space Flight Center, Greenbelt, MD, USALaboratoire d'Aérologie, CNRS and Université Paul Sabatier, Université de Toulouse, Toulouse, FranceNational Center for Atmospheric Research, Boulder, CO, USASchool of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USANOAA Chemical Science Laboratory, Boulder, CO, USA<p>Ozone is a key constituent of the troposphere, where it drives photochemical processes, impacts air quality, and acts as a climate forcer. Large-scale in situ observations of ozone commensurate with the grid resolution of current Earth system models are necessary to validate model outputs and satellite retrievals. In this paper, we examine measurements from the Atmospheric Tomography (ATom; four deployments in 2016–2018) and the HIAPER Pole-to-Pole Observations (HIPPO; five deployments in 2009–2011) experiments, two global-scale airborne campaigns covering the Pacific and Atlantic basins.</p> <p>ATom and HIPPO represent the first global-scale, vertically resolved measurements of <span class="inline-formula">O<sub>3</sub></span> distributions throughout the troposphere, with HIPPO sampling the atmosphere over the Pacific and ATom sampling both the Pacific and Atlantic. Given the relatively limited temporal resolution of these two campaigns, we first compare ATom and HIPPO ozone data to longer-term observational records to establish the representativeness of our dataset. We show that these two airborne campaigns captured on average 53&thinsp;%, 54&thinsp;%, and 38&thinsp;% of the ozone variability in the marine boundary layer, free troposphere, and upper troposphere–lower stratosphere (UTLS), respectively, at nine well-established ozonesonde sites. Additionally, ATom captured the most frequent ozone concentrations measured by regular commercial aircraft flights in the northern Atlantic UTLS. We then use the repeated<span id="page10612"/> vertical profiles from these two campaigns to confirm and extend the existing knowledge of tropospheric ozone spatial and vertical distributions throughout the remote troposphere. We highlight a clear hemispheric gradient, with greater ozone in the Northern Hemisphere, consistent with greater precursor emissions and consistent with previous modeling and satellite studies. We also show that the ozone distribution below 8&thinsp;km was similar in the extra-tropics of the Atlantic and Pacific basins, likely due to zonal circulation patterns. However, twice as much ozone was found in the tropical Atlantic as in the tropical Pacific, due to well-documented dynamical patterns transporting continental air masses over the Atlantic. Finally, we show that the seasonal variability of tropospheric ozone over the Pacific and the Atlantic basins is driven year-round by transported continental plumes and photochemistry, and the vertical distribution is driven by photochemistry and mixing with stratospheric air. This new dataset provides additional constraints for global climate and chemistry models to improve our understanding of both ozone production and loss processes in remote regions, as well as the influence of anthropogenic emissions on baseline ozone.</p>https://acp.copernicus.org/articles/20/10611/2020/acp-20-10611-2020.pdf
spellingShingle I. Bourgeois
I. Bourgeois
J. Peischl
J. Peischl
C. R. Thompson
C. R. Thompson
K. C. Aikin
K. C. Aikin
T. Campos
H. Clark
R. Commane
B. Daube
G. W. Diskin
J. W. Elkins
R.-S. Gao
A. Gaudel
A. Gaudel
E. J. Hintsa
E. J. Hintsa
B. J. Johnson
R. Kivi
K. McKain
K. McKain
F. L. Moore
F. L. Moore
D. D. Parrish
D. D. Parrish
R. Querel
E. Ray
E. Ray
R. Sánchez
C. Sweeney
D. W. Tarasick
A. M. Thompson
V. Thouret
J. C. Witte
S. C. Wofsy
T. B. Ryerson
Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
Atmospheric Chemistry and Physics
title Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
title_full Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
title_fullStr Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
title_full_unstemmed Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
title_short Global-scale distribution of ozone in the remote troposphere from the ATom and HIPPO airborne field missions
title_sort global scale distribution of ozone in the remote troposphere from the atom and hippo airborne field missions
url https://acp.copernicus.org/articles/20/10611/2020/acp-20-10611-2020.pdf
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