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Yan Q, Wang Y, Cheng Y, Li J. Summertime Clean-Background Ozone Concentrations Derived from Ozone Precursor Relationships are Lower than Previous Estimates in the Southeast United States. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2021; 55:12852-12861. [PMID: 34546042 DOI: 10.1021/acs.est.1c03035] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/13/2023]
Abstract
Background ozone in this study is defined as the amount of ozone that is not affected by the emissions of ozone precursors in the region of study and is transported from the distant troposphere or the stratosphere. It is one of the factors that must be considered in regional ozone control strategies. Different methods have been applied to define the background ozone level. We develop a new method based on the O3-CO-HCHO relationships, which can be applied to both observation and modeling data for regions with high isoprene emission ozone, such as the Southeast United States. We make use of the extensive aircraft and surface observations in the Southeast in the summer of 2013. Compared to the diagnostic results using the relationship of O3-NOz (total reactive nitrogen excluding nitrogen oxides), zero-emission (model-only), and 5th percentile methods, the new method is most consistent using observation or model data and the resulting background ozone concentrations are 4-50% lower than the other methods for field campaigns. Using this method, we find that the summertime background ozone at the surface is in the range of 10-15 ppbv in the inland areas of the Southeast, which is lower than that reported in previous studies. This background ozone tends to increase from urban centers to rural regions and from the surface to higher altitude due to changing ozone lifetime driven by anthropogenic emissions and dry deposition to the surface. The better quantification of background ozone using the new method highlights the importance of the contributions by natural emissions to ozone and the necessity to control anthropogenic emissions in ozone nonattainment areas of the Southeast.
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Affiliation(s)
- Qiyang Yan
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, United States
| | - Yuhang Wang
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, United States
| | - Ye Cheng
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, United States
| | - Jianfeng Li
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, United States
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Sorooshian A, Corral AF, Braun RA, Cairns B, Crosbie E, Ferrare R, Hair J, Kleb MM, Mardi AH, Maring H, McComiskey A, Moore R, Painemal D, Jo Scarino A, Schlosser J, Shingler T, Shook M, Wang H, Zeng X, Ziemba L, Zuidema P. Atmospheric Research Over the Western North Atlantic Ocean Region and North American East Coast: A Review of Past Work and Challenges Ahead. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2020; 125:10.1029/2019jd031626. [PMID: 32699733 PMCID: PMC7375207 DOI: 10.1029/2019jd031626] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/12/2019] [Accepted: 01/21/2020] [Indexed: 05/26/2023]
Abstract
Decades of atmospheric research have focused on the Western North Atlantic Ocean (WNAO) region because of its unique location that offers accessibility for airborne and ship measurements, gradients in important atmospheric parameters, and a range of meteorological regimes leading to diverse conditions that are poorly understood. This work reviews these scientific investigations for the WNAO region, including the East Coast of North America and the island of Bermuda. Over 50 field campaigns and long-term monitoring programs, in addition to 715 peer-reviewed publications between 1946 and 2019 have provided a firm foundation of knowledge for these areas. Of particular importance in this region has been extensive work at the island of Bermuda that is host to important time series records of oceanic and atmospheric variables. Our review categorizes WNAO atmospheric research into eight major categories, with some studies fitting into multiple categories (relative %): Aerosols (25%), Gases (24%), Development/Validation of Techniques, Models, and Retrievals (18%), Meteorology and Transport (9%), Air-Sea Interactions (8%), Clouds/Storms (8%), Atmospheric Deposition (7%), and Aerosol-Cloud Interactions (2%). Recommendations for future research are provided in the categories highlighted above.
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Affiliation(s)
- Armin Sorooshian
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ
| | - Andrea F. Corral
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | - Rachel A. Braun
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | - Brian Cairns
- NASA Goddard Institute for Space Studies, New York, NY
| | - Ewan Crosbie
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | | | | | | | - Ali Hossein Mardi
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | | | | | | | - David Painemal
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | - Amy Jo Scarino
- NASA Langley Research Center, Hampton, VA
- Science Systems and Applications, Inc., Hampton, VA
| | - Joseph Schlosser
- Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ
| | | | | | - Hailong Wang
- Atmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA
| | - Xubin Zeng
- Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ
| | | | - Paquita Zuidema
- Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL
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Jaeglé L, Wood R, Wargan K. Multi-year composite view of ozone enhancements and stratosphere-to-troposphere transport in dry intrusions of northern hemisphere extratropical cyclones. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2017; 122:13436-13457. [PMID: 29479506 PMCID: PMC5823518 DOI: 10.1002/2017jd027656] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/08/2023]
Abstract
We examine the role of extratropical cyclones in stratosphere-to-troposphere (STT) exchange with cyclone-centric composites of O3 retrievals from the Microwave Limb Sounder (MLS) and the Tropospheric Emission Spectrometer (TES), contrasting them to composites obtained with the Modern-Era Retrospective-analysis for Research and Applications (MERRA and MERRA-2) reanalyses and the GEOS-Chem chemical transport model. We identify 15,978 extratropical cyclones in the northern hemisphere (NH) for 2005-2012. The lowermost stratosphere (261 hPa) and middle troposphere (424 hPa) composites feature a 1,000 km-wide O3 enhancement in the dry intrusion (DI) airstream to the southwest of the cyclone center, coinciding with a lowered tropopause, enhanced potential vorticity, and decreased H2O. MLS composites at 261 hPa show that the DI O3 enhancements reach a 210 ppbv maximum in April. At 424 hPa, TES composites display maximum O3 enhancements of 27 ppbv in May. The magnitude and seasonality of these enhancements are captured by MERRA and MERRA-2, but GEOS-Chem is a factor of two too low. The MERRA-2 composites show that the O3-rich DI forms a vertically aligned structure between 300 and 800 hPa, wrapping cyclonically with the warm conveyor belt. In winter and spring DIs, O3 is enhanced by 100 ppbv or 100-130% at 300 hPa, with significant enhancements below 500 hPa (6-20 ppbv or 15-30%). We estimate that extratropical cyclones result in a STT flux of 119±56 Tg O3 yr-1, accounting for 42±20 % of the NH extratropical O3 STT flux. The STT flux in cyclones displays a strong dependence on westerly 300 hPa wind speeds.
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Affiliation(s)
- Lyatt Jaeglé
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA
| | - Robert Wood
- Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA
| | - Krzysztof Wargan
- Science Systems and Applications Inc., Lanham, Maryland, USA
- Global Modeling and Assimilation Office, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
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Knowland KE, Doherty RM, Hodges KI, Ott LE. The influence of mid-latitude cyclones on European background surface ozone. ATMOSPHERIC CHEMISTRY AND PHYSICS 2017; 17:12421-12447. [PMID: 32714379 PMCID: PMC7380074 DOI: 10.5194/acp-17-12421-2017] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/01/2023]
Abstract
The relationship between springtime mid-latitude cyclones and background ozone (O3) is explored using a combination of observational and reanalysis data sets. First, the relationship between surface O3 observations at two rural monitoring sites on the west coast of Europe - Mace Head, Ireland and Monte Velho, Portugal - and cyclone track frequency in the surrounding regions is examined. Second, detailed case study examination of four individual mid-latitude cyclones and the influence of the associated frontal passage on surface O3 is performed. Cyclone tracks have a greater influence on the O3 measurements at the more northern coastal European station, Mace Head, located within the main North Atlantic (NA) storm track. In particular, when cyclones track north of 53° N, there is a significant relationship with high levels of surface O3 (> 75th percentile). The further away a cyclone is from the NA storm track, the more likely it will be associated with both high and low (< 25th percentile) levels of O3 at the observation site during the cyclone's life cycle. The results of the four case studies demonstrate a) the importance of the passage of a cyclone's cold front in relation to surface O3 measurements, b) the ability of mid-latitude cyclones to bring down high levels of O3 from the stratosphere and c) that accompanying surface high pressure systems and their associated transport pathways play an important role in the temporal variability of surface O3. The main source of high O3 to these two sites in springtime is from the stratosphere, either from direct injection into the cyclone or associated with aged airstreams from decaying downstream cyclones that can become entrained and descend toward the surface within new cyclones over the NA region.
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Affiliation(s)
- K. Emma Knowland
- Universities Space Research Association (USRA)/Goddard Earth Science Technology & Research (GESTAR)
- Global Modeling and Assimilation Office (GMAO), NASA Goddard Space Flight Center (GSFC), Greenbelt, Maryland, USA
| | - Ruth M. Doherty
- School of Geosciences, University of Edinburgh, Edinburgh, UK
| | | | - Lesley E. Ott
- Global Modeling and Assimilation Office (GMAO), NASA Goddard Space Flight Center (GSFC), Greenbelt, Maryland, USA
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Choi HD, Liu H, Crawford JH, Considine DB, Allen DJ, Duncan BN, Horowitz LW, Rodriguez JM, Strahan SE, Zhang L, Liu X, Damon MR, Steenrod SD. Global O 3-CO Correlations in a Chemistry and Transport Model During July-August: Evaluation with TES Satellite Observations and Sensitivity to Input Meteorological Data and Emissions. ATMOSPHERIC CHEMISTRY AND PHYSICS 2017; 17:8429-8452. [PMID: 32457810 PMCID: PMC7250209 DOI: 10.5194/acp-17-8429-2017] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/31/2023]
Abstract
We examine the capability of the Global Modeling Initiative (GMI) chemistry and transport model to reproduce global mid-tropospheric (618hPa) O3-CO correlations determined by the measurements from Tropospheric Emission Spectrometer (TES) aboard NASA's Aura satellite during boreal summer (July-August). The model is driven by three meteorological data sets (fvGCM with sea surface temperature for 1995, GEOS4-DAS for 2005, and MERRA for 2005), allowing us to examine the sensitivity of model O3-CO correlations to input meteorological data. Model simulations of radionuclide tracers (222Rn, 210Pb, and 7Be) are used to illustrate the differences in transport-related processes among the meteorological data sets. Simulated O3 values are evaluated with climatological ozone profiles from ozonesonde measurements and satellite tropospheric O3 columns. Despite the fact that three simulations show significantly different global and regional distributions of O3 and CO concentrations, all simulations show similar patterns of O3-CO correlations on a global scale. These patterns are consistent with those derived from TES observations, except in the tropical easterly biomass burning outflow regions. Discrepancies in regional O3-CO correlation patterns in the three simulations may be attributed to differences in convective transport, stratospheric influence, and subsidence, among other processes. To understand how various emissions drive global O3-CO correlation patterns, we examine the sensitivity of GMI/MERRA model-calculated O3 and CO concentrations and their correlations to emission types (fossil fuel, biomass burning, biogenic, and lightning NOx emissions). Fossil fuel and biomass burning emissions are mainly responsible for the strong positive O3-CO correlations over continental outflow regions in both hemispheres. Biogenic emissions have a relatively smaller impact on O3-CO correlations than other emissions, but are largely responsible for the negative correlations over the tropical eastern Pacific, reflecting the fact that O3 is consumed and CO generated during the atmospheric oxidation process of isoprene under low NOx conditions. We find that lightning NOx emissions degrade both positive correlations at mid-/high- latitudes and negative correlations in the tropics because ozone production downwind of lightning NOx emissions is not directly related to the emission and transport of CO. Our study concludes that O3-CO correlations may be used effectively to constrain the sources of regional tropospheric O3 in global 3-D models, especially for those regions where convective transport of pollution plays an important role.
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Affiliation(s)
| | - Hongyu Liu
- National Institute of Aerospace, Hampton, VA
| | | | - David B. Considine
- NASA Langley Research Center, Hampton, VA
- Now at NASA Headquarters, Washington, D.C
| | | | | | | | | | - Susan E. Strahan
- NASA Goddard Space Flight Center, Greenbelt, MD
- Universities Space Research Association, Columbia, MD
| | - Lin Zhang
- Harvard University, Cambridge, MA
- Now at Peking University, Beijing, China
| | | | - Megan R. Damon
- NASA Goddard Space Flight Center, Greenbelt, MD
- Science Systems and Applications, Inc., Lanham, MD
| | - Stephen D. Steenrod
- NASA Goddard Space Flight Center, Greenbelt, MD
- Universities Space Research Association, Columbia, MD
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6
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Mercury Plumes in the Global Upper Troposphere Observed during Flights with the CARIBIC Observatory from May 2005 until June 2013. ATMOSPHERE 2014. [DOI: 10.3390/atmos5020342] [Citation(s) in RCA: 22] [Impact Index Per Article: 2.2] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
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Cooper OR, Gao RS, Tarasick D, Leblanc T, Sweeney C. Long-term ozone trends at rural ozone monitoring sites across the United States, 1990-2010. ACTA ACUST UNITED AC 2012. [DOI: 10.1029/2012jd018261] [Citation(s) in RCA: 139] [Impact Index Per Article: 11.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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8
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Pfister GG, Emmons LK, Hess PG, Lamarque JF, Thompson AM, Yorks JE. Analysis of the Summer 2004 ozone budget over the United States using Intercontinental Transport Experiment Ozonesonde Network Study (IONS) observations and Model of Ozone and Related Tracers (MOZART-4) simulations. ACTA ACUST UNITED AC 2008. [DOI: 10.1029/2008jd010190] [Citation(s) in RCA: 47] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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9
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Hegarty J, Mao H, Talbot R. Synoptic controls on summertime surface ozone in the northeastern United States. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd008170] [Citation(s) in RCA: 50] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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10
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Auvray M, Bey I, Llull E, Schultz MG, Rast S. A model investigation of tropospheric ozone chemical tendencies in long-range transported pollution plumes. ACTA ACUST UNITED AC 2007. [DOI: 10.1029/2006jd007137] [Citation(s) in RCA: 32] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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11
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Leclair De Bellevue J, Réchou A, Baray JL, Ancellet G, Diab RD. Signatures of stratosphere to troposphere transport near deep convective events in the southern subtropics. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2005jd006947] [Citation(s) in RCA: 20] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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12
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Price HU, Jaffe DA, Cooper OR, Doskey PV. Photochemistry, ozone production, and dilution during long-range transport episodes from Eurasia to the northwest United States. ACTA ACUST UNITED AC 2004. [DOI: 10.1029/2003jd004400] [Citation(s) in RCA: 54] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Heather U. Price
- Department of Chemistry; University of Washington; Seattle Washington USA
- Interdisciplinary Arts and Sciences; University of Washington; Bothell Washington USA
| | - Daniel A. Jaffe
- Interdisciplinary Arts and Sciences; University of Washington; Bothell Washington USA
| | - Owen R. Cooper
- Cooperative Institute for Research in Environmental Sciences; NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - Paul V. Doskey
- Environmental Research Division; Argonne National Laboratory; Argonne Illinois USA
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Cooper O, Forster C, Parrish D, Dunlea E, Hübler G, Fehsenfeld F, Holloway J, Oltmans S, Johnson B, Wimmers A, Horowitz L. On the life cycle of a stratospheric intrusion and its dispersion into polluted warm conveyor belts. ACTA ACUST UNITED AC 2004. [DOI: 10.1029/2003jd004006] [Citation(s) in RCA: 70] [Impact Index Per Article: 3.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- O. Cooper
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - C. Forster
- Department of Ecology; Technical University of Munich; Freising-Weihenstephan Germany
| | - D. Parrish
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - E. Dunlea
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - G. Hübler
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | | | - J. Holloway
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - S. Oltmans
- NOAA Climate Monitoring and Diagnostics Laboratory; Boulder Colorado USA
| | - B. Johnson
- NOAA Climate Monitoring and Diagnostics Laboratory; Boulder Colorado USA
| | - A. Wimmers
- Department of Environmental Sciences; University of Virginia; Charlottesville Virginia USA
| | - L. Horowitz
- NOAA Geophysical Fluid Dynamics Laboratory; Princeton New Jersey USA
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Cooper OR, Forster C, Parrish D, Trainer M, Dunlea E, Ryerson T, Hübler G, Fehsenfeld F, Nicks D, Holloway J, de Gouw J, Warneke C, Roberts JM, Flocke F, Moody J. A case study of transpacific warm conveyor belt transport: Influence of merging airstreams on trace gas import to North America. ACTA ACUST UNITED AC 2004. [DOI: 10.1029/2003jd003624] [Citation(s) in RCA: 145] [Impact Index Per Article: 7.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- O. R. Cooper
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - C. Forster
- Department of Ecology; Technical University of Munich; Freising-Weihenstephan Germany
| | - D. Parrish
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - M. Trainer
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - E. Dunlea
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - T. Ryerson
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - G. Hübler
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | | | - D. Nicks
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - J. Holloway
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - J. de Gouw
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - C. Warneke
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - J. M. Roberts
- Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA
- NOAA Aeronomy Laboratory; Boulder Colorado USA
| | - F. Flocke
- National Center for Atmospheric Research; Boulder Colorado USA
| | - J. Moody
- Department of Environmental Sciences; University of Virginia; Charlottesville Virginia USA
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Crawford J, Olson J, Davis D, Chen G, Barrick J, Shetter R, Lefer B, Jordan C, Anderson B, Clarke A, Sachse G, Blake D, Singh H, Sandolm S, Tan D, Kondo Y, Avery M, Flocke F, Eisele F, Mauldin L, Zondlo M, Brune W, Harder H, Martinez M, Talbot R, Bandy A, Thornton D. Clouds and trace gas distributions during TRACE-P. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2002jd003177] [Citation(s) in RCA: 27] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- J. Crawford
- NASA Langley Research Center; Hampton Virginia USA
| | - J. Olson
- NASA Langley Research Center; Hampton Virginia USA
| | - D. Davis
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - G. Chen
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - J. Barrick
- NASA Langley Research Center; Hampton Virginia USA
| | - R. Shetter
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - B. Lefer
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - C. Jordan
- NASA Langley Research Center; Hampton Virginia USA
| | - B. Anderson
- NASA Langley Research Center; Hampton Virginia USA
| | - A. Clarke
- School of Ocean and Earth Science and Technology; University of Hawaii; Honolulu Hawaii USA
| | - G. Sachse
- NASA Langley Research Center; Hampton Virginia USA
| | - D. Blake
- Department of Chemistry; University of California; Irvine California USA
| | - H. Singh
- NASA Ames Research Center; Moffett Field California USA
| | - S. Sandolm
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - D. Tan
- School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA
| | - Y. Kondo
- Research Center for Advanced Science and Technology; University of Tokyo; Tokyo Japan
| | - M. Avery
- NASA Langley Research Center; Hampton Virginia USA
| | - F. Flocke
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - F. Eisele
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - L. Mauldin
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - M. Zondlo
- Atmospheric Chemistry Division; National Center for Atmospheric Research; Boulder Colorado USA
| | - W. Brune
- Department of Meteorology; Pennsylvania State University; University Park Pennsylvania USA
| | - H. Harder
- Department of Meteorology; Pennsylvania State University; University Park Pennsylvania USA
| | - M. Martinez
- Department of Meteorology; Pennsylvania State University; University Park Pennsylvania USA
| | - R. Talbot
- Institute for the Study of Earth, Oceans, and Space; University of New Hampshire; Durham New Hampshire USA
| | - A. Bandy
- Department of Chemistry; Drexel University; Philadelphia Pennsylvania USA
| | - D. Thornton
- Department of Chemistry; Drexel University; Philadelphia Pennsylvania USA
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