1
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Zhang J, Gong X, Crosbie E, Diskin G, Froyd K, Hall S, Kupc A, Moore R, Peischl J, Rollins A, Schwarz J, Shook M, Thompson C, Ullmann K, Williamson C, Wisthaler A, Xu L, Ziemba L, Brock CA, Wang J. Stratospheric air intrusions promote global-scale new particle formation. Science 2024; 385:210-216. [PMID: 38991080 DOI: 10.1126/science.adn2961] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/05/2023] [Accepted: 05/13/2024] [Indexed: 07/13/2024]
Abstract
New particle formation in the free troposphere is a major source of cloud condensation nuclei globally. The prevailing view is that in the free troposphere, new particles are formed predominantly in convective cloud outflows. We present another mechanism using global observations. We find that during stratospheric air intrusion events, the mixing of descending ozone-rich stratospheric air with more moist free tropospheric background results in elevated hydroxyl radical (OH) concentrations. Such mixing is most prevalent near the tropopause where the sulfur dioxide (SO2) mixing ratios are high. The combination of elevated SO2 and OH levels leads to enhanced sulfuric acid concentrations, promoting particle formation. Such new particle formation occurs frequently and over large geographic regions, representing an important particle source in the midlatitude free troposphere.
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Affiliation(s)
- Jiaoshi Zhang
- Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA
| | - Xianda Gong
- Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA
| | - Ewan Crosbie
- NASA Langley Research Center, Hampton, VA, USA
- Science Systems and Applications, Inc., Hampton, VA, USA
| | | | - Karl Froyd
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Samuel Hall
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - Agnieszka Kupc
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
- Faculty of Physics, Aerosol Physics and Environmental Physics, University of Vienna, Vienna, Austria
| | | | - Jeff Peischl
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Andrew Rollins
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Joshua Schwarz
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | | | - Chelsea Thompson
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Kirk Ullmann
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
| | - Christina Williamson
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
- Climate Research Programme, Finnish Meteorological Institute, Helsinki, Finland
- Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki, Finland
| | - Armin Wisthaler
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Department of Chemistry, University of Oslo, Oslo, Norway
| | - Lu Xu
- Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA
| | - Luke Ziemba
- NASA Langley Research Center, Hampton, VA, USA
| | - Charles A Brock
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
| | - Jian Wang
- Center for Aerosol Science and Engineering, Department of Energy, Environmental and Chemical Engineering, Washington University in St. Louis, St. Louis, MO, USA
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2
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Ferracci V, Weber J, Bolas CG, Robinson AD, Tummon F, Rodríguez-Ros P, Cortés-Greus P, Baccarini A, Jones RL, Galí M, Simó R, Schmale J, Harris NRP. Atmospheric isoprene measurements reveal larger-than-expected Southern Ocean emissions. Nat Commun 2024; 15:2571. [PMID: 38519467 PMCID: PMC10959939 DOI: 10.1038/s41467-024-46744-4] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/18/2023] [Accepted: 03/05/2024] [Indexed: 03/25/2024] Open
Abstract
Isoprene is a key trace component of the atmosphere emitted by vegetation and other organisms. It is highly reactive and can impact atmospheric composition and climate by affecting the greenhouse gases ozone and methane and secondary organic aerosol formation. Marine fluxes are poorly constrained due to the paucity of long-term measurements; this in turn limits our understanding of isoprene cycling in the ocean. Here we present the analysis of isoprene concentrations in the atmosphere measured across the Southern Ocean over 4 months in the summertime. Some of the highest concentrations ( >500 ppt) originated from the marginal ice zone in the Ross and Amundsen seas, indicating the marginal ice zone is a significant source of isoprene at high latitudes. Using the United Kingdom Earth System Model we show that current estimates of sea-to-air isoprene fluxes underestimate observed isoprene by a factor >20. A daytime source of isoprene is required to reconcile models with observations. The model presented here suggests such an increase in isoprene emissions would lead to >8% decrease in the hydroxyl radical in regions of the Southern Ocean, with implications for our understanding of atmospheric oxidation and composition in remote environments, often used as proxies for the pre-industrial atmosphere.
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Affiliation(s)
- Valerio Ferracci
- Cranfield Environment Centre, Cranfield University, College Road, Cranfield, UK.
- National Physical Laboratory, Hampton Road, Teddington, UK.
| | - James Weber
- School of Biosciences, University of Sheffield, Sheffield, UK.
- Dept of Meteorology, University of Reading, Reading, UK.
| | - Conor G Bolas
- Department of Chemistry, University of Cambridge, Lensfield Road, Cambridge, UK
- ITOPF, Old Broad Street, London, UK
| | - Andrew D Robinson
- Department of Chemistry, University of Cambridge, Lensfield Road, Cambridge, UK
- Schlumberger Cambridge Research, Madingley Road, Cambridge, UK
| | - Fiona Tummon
- Swiss Federal Office for Meteorology and Climatology MeteoSwiss, Payerne, Switzerland
| | - Pablo Rodríguez-Ros
- Institut de Ciències del Mar (ICM-CSIC), Barcelona, Catalonia, Spain
- Marilles Foundation, Bisbe Perelló, Palma, Mallorca, Spain
| | - Pau Cortés-Greus
- Institut de Ciències del Mar (ICM-CSIC), Barcelona, Catalonia, Spain
| | - Andrea Baccarini
- Extreme Environments Research Laboratory, École Polytechnique Fédérale de Lausanne, Lausanne, Switzerland
- Laboratory of atmospheric processes and their impact, École Polytechnique Fédérale de Lausanne, Lausanne, Switzerland
| | - Roderic L Jones
- Department of Chemistry, University of Cambridge, Lensfield Road, Cambridge, UK
| | - Martí Galí
- Institut de Ciències del Mar (ICM-CSIC), Barcelona, Catalonia, Spain
| | - Rafel Simó
- Institut de Ciències del Mar (ICM-CSIC), Barcelona, Catalonia, Spain
| | - Julia Schmale
- Extreme Environments Research Laboratory, École Polytechnique Fédérale de Lausanne, Lausanne, Switzerland
| | - Neil R P Harris
- Cranfield Environment Centre, Cranfield University, College Road, Cranfield, UK
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3
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Baublitz CB, Fiore AM, Ludwig SM, Nicely JM, Wolfe GM, Murray LT, Commane R, Prather MJ, Anderson DC, Correa G, Duncan BN, Follette-Cook M, Westervelt DM, Bourgeois I, Brune WH, Bui TP, DiGangi JP, Diskin GS, Hall SR, McKain K, Miller DO, Peischl J, Thames AB, Thompson CR, Ullmann K, Wofsy SC. An observation-based, reduced-form model for oxidation in the remote marine troposphere. Proc Natl Acad Sci U S A 2023; 120:e2209735120. [PMID: 37579162 PMCID: PMC10451388 DOI: 10.1073/pnas.2209735120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/07/2022] [Accepted: 06/26/2023] [Indexed: 08/16/2023] Open
Abstract
The hydroxyl radical (OH) fuels atmospheric chemical cycling as the main sink for methane and a driver of the formation and loss of many air pollutants, but direct OH observations are sparse. We develop and evaluate an observation-based proxy for short-term, spatial variations in OH (ProxyOH) in the remote marine troposphere using comprehensive measurements from the NASA Atmospheric Tomography (ATom) airborne campaign. ProxyOH is a reduced form of the OH steady-state equation representing the dominant OH production and loss pathways in the remote marine troposphere, according to box model simulations of OH constrained with ATom observations. ProxyOH comprises only eight variables that are generally observed by routine ground- or satellite-based instruments. ProxyOH scales linearly with in situ [OH] spatial variations along the ATom flight tracks (median r2 = 0.90, interquartile range = 0.80 to 0.94 across 2-km altitude by 20° latitudinal regions). We deconstruct spatial variations in ProxyOH as a first-order approximation of the sensitivity of OH variations to individual terms. Two terms modulate within-region ProxyOH variations-water vapor (H2O) and, to a lesser extent, nitric oxide (NO). This implies that a limited set of observations could offer an avenue for observation-based mapping of OH spatial variations over much of the remote marine troposphere. Both H2O and NO are expected to change with climate, while NO also varies strongly with human activities. We also illustrate the utility of ProxyOH as a process-based approach for evaluating intermodel differences in remote marine tropospheric OH.
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Affiliation(s)
- Colleen B. Baublitz
- Department of Earth and Environmental Sciences, Columbia University, New York, NY10027
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
| | - Arlene M. Fiore
- Department of Earth and Environmental Sciences, Columbia University, New York, NY10027
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
| | - Sarah M. Ludwig
- Department of Earth and Environmental Sciences, Columbia University, New York, NY10027
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
| | - Julie M. Nicely
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD20740
- Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration Goddard Space Flight Center, Greenbelt, MD20771
| | - Glenn M. Wolfe
- Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration Goddard Space Flight Center, Greenbelt, MD20771
| | - Lee T. Murray
- Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY14627
| | - Róisín Commane
- Department of Earth and Environmental Sciences, Columbia University, New York, NY10027
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
| | - Michael J. Prather
- Department of Earth System Science, University of California, Irvine, CA92697
| | - Daniel C. Anderson
- Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration Goddard Space Flight Center, Greenbelt, MD20771
- Goddard Earth Sciences Technology and Research II, University of Maryland Baltimore County, Baltimore, MD21250
| | - Gustavo Correa
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
| | - Bryan N. Duncan
- Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration Goddard Space Flight Center, Greenbelt, MD20771
| | - Melanie Follette-Cook
- Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration Goddard Space Flight Center, Greenbelt, MD20771
- Goddard Earth Sciences Technology and Research II, Morgan State University, Baltimore, MD21251
| | - Daniel M. Westervelt
- Division of Ocean and Climate Physics, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY10964
- National Aeronautics and Space Administration Goddard Institute for Space Studies, New York, NY10025
| | - Ilann Bourgeois
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO80309
- National Oceanic and Atmospheric Administration Chemical Sciences Laboratory, Boulder, CO80305
| | - William H. Brune
- Department of Meteorology and Atmospheric Science, Pennsylvania State University, University Park, PA16802
| | - T. Paul Bui
- Atmospheric Science Branch, National Aeronautics and Space Administration Ames Research Center, Moffett Field, CA94035
| | - Joshua P. DiGangi
- National Aeronautics and Space Administration Langley Research Center, Hampton, VA23666
| | - Glenn S. Diskin
- National Aeronautics and Space Administration Langley Research Center, Hampton, VA23666
| | - Samuel R. Hall
- Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO80307
| | - Kathryn McKain
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO80309
- National Oceanic and Atmospheric Administration Global Monitoring Laboratory, Boulder, CO80305
| | - David O. Miller
- Department of Meteorology and Atmospheric Science, Pennsylvania State University, University Park, PA16802
| | - Jeff Peischl
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO80309
- National Oceanic and Atmospheric Administration Chemical Sciences Laboratory, Boulder, CO80305
| | - Alexander B. Thames
- Department of Meteorology and Atmospheric Science, Pennsylvania State University, University Park, PA16802
| | - Chelsea R. Thompson
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO80309
- National Oceanic and Atmospheric Administration Chemical Sciences Laboratory, Boulder, CO80305
| | - Kirk Ullmann
- Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO80307
| | - Steven C. Wofsy
- Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA02138
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4
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Tassone A, Magand O, Naccarato A, Martino M, Amico D, Sprovieri F, Leuridan H, Bertrand Y, Ramonet M, Pirrone N, Dommergue A. Seven-year monitoring of mercury in wet precipitation and atmosphere at the Amsterdam Island GMOS station. Heliyon 2023; 9:e14608. [PMID: 37020937 PMCID: PMC10068122 DOI: 10.1016/j.heliyon.2023.e14608] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/20/2022] [Revised: 03/05/2023] [Accepted: 03/13/2023] [Indexed: 03/19/2023] Open
Abstract
Mercury (Hg) fate and transport research requires more effort to obtain a deep knowledge of its biogeochemical cycle, particularly in the Southern Hemisphere and Tropics that are still missing of distributed monitoring sites. Continuous monitoring of atmospheric Hg concentrations and trend worldwide is relevant for the effectiveness evaluation of the Minamata Convention on Mercury (MCM) actions. In this context, Gaseous Elemental Mercury (GEM) and total mercury (THg) in precipitations were monitored from 2013 to 2019 at the Amsterdam Island Observatory (AMS - 37°48'S, 77°34'E) to provide insights into the Hg pathway in the remote southern Indian Ocean, also considering ancillary dataset of Rn-222, CO2, CO, and CH4. GEM average concentration was 1.06 ± 0.07 ng m-3, with a slight increase during the austral winter due to both higher wind speed over the surface ocean and contributions from southern Africa. In wet depositions, THg average concentration was 2.39 ± 1.17 ng L-1, whereas the annual flux averaged 2.04 ± 0.80 μg m-2 year-1. In general, both GEM and Volume-Weighted Mean Concentration (VWMC) of THg did not show an increasing/decreasing trend over the seven-year period, suggesting a substantial lack of evolution about emission of Hg reaching AMS. Air masses Cluster Analysis and Potential Source Contribution Function showed that oceanic evasion was the main Hg contributor at AMS, while further contributions were attributable to long-range transport events from southern Africa, particularly when the occurrence of El Niño increased the frequency of wildfires.
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Affiliation(s)
- Antonella Tassone
- CNR-Institute of Atmospheric Pollution Research (CNR-IIA), Rende, Italy
- Corresponding author. CNR-Institute of Atmospheric Pollution Research, Rende, Italy.
| | - Olivier Magand
- Institut des Géosciences de l’Environnement, Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, 38400, Grenoble, France
| | - Attilio Naccarato
- CNR-Institute of Atmospheric Pollution Research (CNR-IIA), Rende, Italy
- Department of Chemistry and Chemical Technologies, University of Calabria, Via P. Bucci, Rende, Italy
| | - Maria Martino
- CNR-Institute of Atmospheric Pollution Research (CNR-IIA), Rende, Italy
| | - Domenico Amico
- CNR-Institute of Atmospheric Pollution Research (CNR-IIA), Rende, Italy
| | | | - Hippolyte Leuridan
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE-IPSL (CEA-CNRS-UVSQ), Université Paris-Saclay, 91191, Gif-sur-Yvette, France
| | - Yann Bertrand
- Institut des Géosciences de l’Environnement, Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, 38400, Grenoble, France
| | - Michel Ramonet
- Laboratoire des Sciences du Climat et de l'Environnement, LSCE-IPSL (CEA-CNRS-UVSQ), Université Paris-Saclay, 91191, Gif-sur-Yvette, France
| | - Nicola Pirrone
- CNR-Institute of Atmospheric Pollution Research (CNR-IIA), Rende, Italy
| | - Aurelien Dommergue
- Institut des Géosciences de l’Environnement, Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, 38400, Grenoble, France
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5
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Andersen ST, Carpenter LJ, Reed C, Lee JD, Chance R, Sherwen T, Vaughan AR, Stewart J, Edwards PM, Bloss WJ, Sommariva R, Crilley LR, Nott GJ, Neves L, Read K, Heard DE, Seakins PW, Whalley LK, Boustead GA, Fleming LT, Stone D, Fomba KW. Extensive field evidence for the release of HONO from the photolysis of nitrate aerosols. SCIENCE ADVANCES 2023; 9:eadd6266. [PMID: 36652523 PMCID: PMC9848427 DOI: 10.1126/sciadv.add6266] [Citation(s) in RCA: 12] [Impact Index Per Article: 12.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/23/2022] [Accepted: 12/19/2022] [Indexed: 06/01/2023]
Abstract
Particulate nitrate ([Formula: see text]) has long been considered a permanent sink for NOx (NO and NO2), removing a gaseous pollutant that is central to air quality and that influences the global self-cleansing capacity of the atmosphere. Evidence is emerging that photolysis of [Formula: see text] can recycle HONO and NOx back to the gas phase with potentially important implications for tropospheric ozone and OH budgets; however, there are substantial discrepancies in "renoxification" photolysis rate constants. Using aircraft and ground-based HONO observations in the remote Atlantic troposphere, we show evidence for renoxification occurring on mixed marine aerosols with an efficiency that increases with relative humidity and decreases with the concentration of [Formula: see text], thus largely reconciling the very large discrepancies in renoxification photolysis rate constants found across multiple laboratory and field studies. Active release of HONO from aerosol has important implications for atmospheric oxidants such as OH and O3 in both polluted and clean environments.
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Affiliation(s)
- Simone T. Andersen
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | - Lucy J. Carpenter
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | | | - James D. Lee
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
- National Centre for Atmospheric Science, University of York, York, UK
| | - Rosie Chance
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | - Tomás Sherwen
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
- National Centre for Atmospheric Science, University of York, York, UK
| | - Adam R. Vaughan
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | - Jordan Stewart
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | - Pete M. Edwards
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
| | - William J. Bloss
- School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
| | - Roberto Sommariva
- School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
| | - Leigh R. Crilley
- School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
| | | | - Luis Neves
- Instituto Nacional de Meteorologia e Geofísica, São Vicente (INMG), Mindelo, Cabo Verde
| | - Katie Read
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York, UK
- National Centre for Atmospheric Science, University of York, York, UK
| | | | | | - Lisa K. Whalley
- FAAM Airborne Laboratory, Cranfield, UK
- School of Chemistry, University of Leeds, Leeds, UK
| | | | | | - Daniel Stone
- School of Chemistry, University of Leeds, Leeds, UK
| | - Khanneh Wadinga Fomba
- Atmospheric Chemistry Department, Leibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germany
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6
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Sedlacek AJ, Lewis ER, Onasch TB, Zuidema P, Redemann J, Jaffe D, Kleinman LI. Using the Black Carbon Particle Mixing State to Characterize the Lifecycle of Biomass Burning Aerosols. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:14315-14325. [PMID: 36200733 DOI: 10.1021/acs.est.2c03851] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/16/2023]
Abstract
The lifecycle of black carbon (BC)-containing particles from biomass burns is examined using aircraft and surface observations of the BC mixing state for plume ages from ∼15 min to 10 days. Because BC is nonvolatile and chemically inert, changes in the mixing state of BC-containing particles are driven solely by changes in particle coating, which is mainly secondary organic aerosol (SOA). The coating mass initially increases rapidly (kgrowth = 0.84 h-1), then remains relatively constant for 1-2 days as plume dilution no longer supports further growth, and then decreases slowly until only ∼30% of the maximum coating mass remains after 10 days (kloss = 0.011 h-1). The mass ratio of coating-to-core for a BC-containing particle with a 100 nm mass-equivalent diameter BC core reaches a maximum of ∼20 after a few hours and drops to ∼5 after 10 days of aging. The initial increase in coating mass can be used to determine SOA formation rates. The slow loss of coating material, not captured in global models, comprises the dominant fraction of the lifecycle of these particles. Coating-to-core mass ratios of BC particles in the stratosphere are much greater than those in the free troposphere indicating a different lifecycle.
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Affiliation(s)
- Arthur J Sedlacek
- Brookhaven National Laboratory, Upton, New York 11973, United States
| | - Ernie R Lewis
- Brookhaven National Laboratory, Upton, New York 11973, United States
| | - Timothy B Onasch
- Aerodyne Research, Inc., Billerica, Massachusetts 01821, United States
| | | | - Jens Redemann
- University of Oklahoma, Norman, Oklahoma 73072, United States
| | - Daniel Jaffe
- University of Washington/Bothell, Bothell, Washington 98011, United States
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7
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Chen X, Millet DB, Neuman JA, Veres PR, Ray EA, Commane R, Daube BC, McKain K, Schwarz JP, Katich JM, Froyd KD, Schill GP, Kim MJ, Crounse JD, Allen HM, Apel EC, Hornbrook RS, Blake DR, Nault BA, Campuzano-Jost P, Jimenez JL, Dibb JE. HCOOH in the remote atmosphere: Constraints from Atmospheric Tomography (ATom) airborne observations. ACS EARTH & SPACE CHEMISTRY 2021; 5:1436-1454. [PMID: 34164590 PMCID: PMC8216292 DOI: 10.1021/acsearthspacechem.1c00049] [Citation(s) in RCA: 6] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/13/2023]
Abstract
Formic acid (HCOOH) is an important component of atmospheric acidity but its budget is poorly understood, with prior observations implying substantial missing sources. Here we combine pole-to-pole airborne observations from the Atmospheric Tomography Mission (ATom) with chemical transport model (GEOS-Chem CTM) and back trajectory analyses to provide the first global in-situ characterization of HCOOH in the remote atmosphere. ATom reveals sub-100 ppt HCOOH concentrations over most of the remote oceans, punctuated by large enhancements associated with continental outflow. Enhancements correlate with known combustion tracers and trajectory-based fire influences. The GEOS-Chem model underpredicts these in-plume HCOOH enhancements, but elsewhere we find no broad indication of a missing HCOOH source in the background free troposphere. We conclude that missing non-fire HCOOH precursors inferred previously are predominantly short-lived. We find indications of a wet scavenging underestimate in the model consistent with a positive HCOOH bias in the tropical upper troposphere. Observations reveal episodic evidence of ocean HCOOH uptake, which is well-captured by GEOS-Chem; however, despite its strong seawater undersaturation HCOOH is not consistently depleted in the remote marine boundary layer. Over fifty fire and mixed plumes were intercepted during ATom with widely varying transit times and source regions. HCOOH:CO normalized excess mixing ratios in these plumes range from 3.4 to >50 ppt/ppb CO and are often over an order of magnitude higher than expected primary emission ratios. HCOOH is thus a major reactive organic carbon reservoir in the aged plumes sampled during ATom, implying important missing pathways for in-plume HCOOH production.
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Affiliation(s)
- Xin Chen
- Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108
| | - Dylan B. Millet
- Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108
| | - J. Andrew Neuman
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
| | | | - Eric A. Ray
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
| | - Róisín Commane
- Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory, Columbia University, New York, NY 10964
| | - Bruce C. Daube
- Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138
| | - Kathryn McKain
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
- NOAA Global Monitoring Laboratory, Boulder, CO 80305
| | | | - Joseph M. Katich
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
| | - Karl D. Froyd
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
| | - Gregory P. Schill
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
| | - Michelle J. Kim
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125
| | - John D. Crounse
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125
| | - Hannah M. Allen
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA 91125
| | - Eric C. Apel
- Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO 80307
| | - Rebecca S. Hornbrook
- Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO 80307
| | - Donald R. Blake
- Department of Chemistry, University of California, Irvine, CA 92697
| | - Benjamin A. Nault
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
- Department of Chemistry, University of Colorado Boulder, Boulder, CO 80309
| | - Pedro Campuzano-Jost
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
- Department of Chemistry, University of Colorado Boulder, Boulder, CO 80309
| | - Jose L. Jimenez
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309
- Department of Chemistry, University of Colorado Boulder, Boulder, CO 80309
| | - Jack E. Dibb
- Earth Systems Research Center/EOS, University of New Hampshire, Durham, NH 03824
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8
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Li Q, Badia A, Fernandez RP, Mahajan AS, López‐Noreña AI, Zhang Y, Wang S, Puliafito E, Cuevas CA, Saiz‐Lopez A. Chemical Interactions Between Ship-Originated Air Pollutants and Ocean-Emitted Halogens. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2021; 126:e2020JD034175. [PMID: 33816042 PMCID: PMC8008258 DOI: 10.1029/2020jd034175] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 10/31/2020] [Revised: 12/09/2020] [Accepted: 12/27/2020] [Indexed: 06/12/2023]
Abstract
Ocean-going ships supply products from one region to another and contribute to the world's economy. Ship exhaust contains many air pollutants and results in significant changes in marine atmospheric composition. The role of reactive halogen species (RHS) in the troposphere has received increasing recognition and oceans are the largest contributors to their atmospheric burden. However, the impact of shipping emissions on RHS and that of RHS on ship-originated air pollutants have not been studied in detail. Here, an updated Weather Research Forecasting coupled with Chemistry model is utilized to explore the chemical interactions between ship emissions and oceanic RHS over the East Asia seas in summer. The emissions and resulting chemical transformations from shipping activities increase the level of NO and NO2 at the surface, increase O3 in the South China Sea, but decrease O3 in the East China Sea. Such changes in pollutants result in remarkable changes in the levels of RHS (>200% increase of chlorine; ∼30% and ∼5% decrease of bromine and iodine, respectively) as well as in their partitioning. The abundant RHS, in turn, reshape the loadings of air pollutants (∼20% decrease of NO and NO2; ∼15% decrease of O3) and those of the oxidants (>10% reduction of OH and HO2; ∼40% decrease of NO3) with marked patterns along the ship tracks. We, therefore, suggest that these important chemical interactions of ship-originated emissions with RHS should be considered in the environmental policy assessments of the role of shipping emissions in air quality and climate.
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Affiliation(s)
- Qinyi Li
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
| | - Alba Badia
- Institute of Environmental Science and Technology (ICTA)Universitat Autònoma de Barcelona (UAB)BarcelonaSpain
| | - Rafael P. Fernandez
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
- Institute for Interdisciplinary Science (ICB)National Research Council (CONICET)FCEN‐UNCuyoMendozaArgentina
| | - Anoop S. Mahajan
- Centre for Climate Change ResearchIndian Institute of Tropical MeteorologyPuneIndia
| | - Ana Isabel López‐Noreña
- Atmospheric and Environmental Studies Group (GEAA)National Technological University (UTN‐FRM)CONICETMendozaArgentina
| | - Yan Zhang
- Department of Environmental Science and EngineeringShanghai Key Laboratory of Atmospheric Particle Pollution and PreventionFudan UniversityShanghaiChina
| | - Shanshan Wang
- Department of Environmental Science and EngineeringShanghai Key Laboratory of Atmospheric Particle Pollution and PreventionFudan UniversityShanghaiChina
| | - Enrique Puliafito
- Atmospheric and Environmental Studies Group (GEAA)National Technological University (UTN‐FRM)CONICETMendozaArgentina
| | - Carlos A. Cuevas
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
| | - Alfonso Saiz‐Lopez
- Department of Atmospheric Chemistry and ClimateInstitute of Physical Chemistry RocasolanoCSICMadridSpain
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9
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Heald CL, Gouw JD, Goldstein AH, Guenther AB, Hayes PL, Hu W, Isaacman-VanWertz G, Jimenez JL, Keutsch FN, Koss AR, Misztal PK, Rappenglück B, Roberts JM, Stevens PS, Washenfelder RA, Warneke C, Young CJ. Contrasting Reactive Organic Carbon Observations in the Southeast United States (SOAS) and Southern California (CalNex). ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:14923-14935. [PMID: 33205951 DOI: 10.1021/acs.est.0c05027] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/11/2023]
Abstract
Despite the central role of reactive organic carbon (ROC) in the formation of secondary species that impact global air quality and climate, our assessment of ROC abundance and impacts is challenged by the diversity of species that contribute to it. We revisit measurements of ROC species made during two field campaigns in the United States: the 2013 SOAS campaign in forested Centreville, AL, and the 2010 CalNex campaign in urban Pasadena, CA. We find that average measured ROC concentrations are about twice as high in Pasadena (73.8 μgCsm-3) than in Centreville (36.5 μgCsm-3). However, the OH reactivity (OHR) measured at these sites is similar (20.1 and 19.3 s-1). The shortfall in OHR when summing up measured contributions is 31%, at Pasadena and 14% at Centreville, suggesting that there may be a larger reservoir of unmeasured ROC at the former site. Estimated O3 production and SOA potential (defined as concentration × yield) are both higher during CalNex than SOAS. This analysis suggests that the ROC in urban California is less reactive, but due to higher concentrations of oxides of nitrogen and hydroxyl radicals, is more efficient in terms of O3 and SOA production, than in the forested southeastern U.S.
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Affiliation(s)
- Colette L Heald
- Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States
| | - Joost de Gouw
- Department of Chemistry, University of Colorado, Boulder, Colorado 80309, United States
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
| | - Allen H Goldstein
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, California 94720, United States
- Department of Civil and Environmental Engineering, University of California, Berkeley, California 94720, United States
| | - Alex B Guenther
- Department of Earth System Science, University of California, Irvine,California 92697, United States
| | - Patrick L Hayes
- Department of Chemistry, University of Colorado, Boulder, Colorado 80309, United States
| | - Weiwei Hu
- Department of Chemistry, University of Colorado, Boulder, Colorado 80309, United States
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
| | - Gabriel Isaacman-VanWertz
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, California 94720, United States
| | - Jose L Jimenez
- Department of Chemistry, University of Colorado, Boulder, Colorado 80309, United States
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
| | - Frank N Keutsch
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138, United States
| | - Abigail R Koss
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado 80305, United States
| | - Pawel K Misztal
- Department of Environmental Science, Policy, and Management, University of California, Berkeley, California 94720, United States
| | - Bernhard Rappenglück
- Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas 77204, United States
| | - James M Roberts
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado 80305, United States
| | - Philip S Stevens
- O'Neill School of Public and Environmental Affairs, Indiana University, Bloomington, Indiana 47405, United States
- Department of Chemistry, Indiana University, Bloomington, Indiana 47405, United States
| | - Rebecca A Washenfelder
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado 80305, United States
| | - Carsten Warneke
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
- Chemical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, Colorado 80305, United States
| | - Cora J Young
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, United States
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