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Li W, Han X, Li J, Lun X, Zhang M. Assessment of surface ozone production in Qinghai, China with satellite-constrained VOCs and NO x emissions. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 905:166602. [PMID: 37659549 DOI: 10.1016/j.scitotenv.2023.166602] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/12/2023] [Revised: 08/05/2023] [Accepted: 08/25/2023] [Indexed: 09/04/2023]
Abstract
The implementation of the western development strategy of China and the migration of air pollutants from eastern China might lead to a rapid increase in volatile organic compounds (VOCs) concentrations in the Qinghai-Tibet Plateau (QTP) and an amplified role of Nitrogen Oxides (NOx) in ozone (O3) pollution. Qinghai province, situated on the northeast of the QTP, had fewer human activities compared to eastern China, while ozone pollution worsened over the years. To better capture recent emission trends and improve the accuracy of O3 simulation in Qinghai, this study proposed a top-down method, which combined the air quality modeling system RAMS-CMAQ, with formaldehyde (HCHO) and nitrogen dioxide (NO2) columns derived from TROPOMI as the constraints to improve the emission estimates of VOCs and NOx in July 2020, respectively. Through a series of sensitivity experiments, better quantified emission estimates of VOCs and NOx were obtained to be 1.33 and 0.34 Tg/yr, 2.5 and 2.1 times larger than the bottom-up ones. The results demonstrated the effectiveness of the top-down method and satellite observations constraints in improving VOCs and NOx emission estimates, resulting in a reduction in the differences between the observed and modeled HCHO and NO2 columns to 0.7 and 0.2 × 1015 molec/cm2, respectively. As a result, the simulated maximum daily 8-h average (MDA8) O3 concentrations increased from 58.9 to 81.6 μg/m3, which were closer to observations (85.4 μg/m3), the normalized mean bias (NMB) and normalized mean error (NME) values of hourly O3 concentrations changed from -24.7 % to -2.9 % and from 29.9 % to 22.3 %, respectively. This study showed the potential of top-down estimates to aide in the development of emission scenarios, which were critical for accurately simulating the O3 pollution and pollution control policy studies.
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Affiliation(s)
- Wen Li
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Xiao Han
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Jialin Li
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
| | - Xiaoxiu Lun
- College of Environmental Science and Engineering, Beijing Forestry University, Beijing 100083, China
| | - Meigen Zhang
- State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China.
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2
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Stewart M, Ohno PE, McKinney K, Martin ST. Prediction of the Response of a Photoionization Detector to a Complex Gaseous Mixture of Volatile Organic Compounds Produced by α-Pinene Oxidation. ACS EARTH & SPACE CHEMISTRY 2023; 7:1956-1970. [PMID: 37876663 PMCID: PMC10592314 DOI: 10.1021/acsearthspacechem.3c00054] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/07/2023] [Revised: 09/19/2023] [Accepted: 09/19/2023] [Indexed: 10/26/2023]
Abstract
Photoionization detectors (PIDs) are lightweight and respond in real time to the concentrations of volatile organic compounds (VOCs), making them suitable for environmental measurements on many platforms. However, the nonselective sensing mechanism of PIDs challenges data interpretation, particularly when exposed to the complex VOC mixtures prevalent in the Earth's atmosphere. Herein, two approaches to this challenge are investigated. In the first, quantum-chemistry calculations are used to estimate photoionization cross sections and ionization potentials of individual species. In the second, machine learning models are trained on these calculated values, as well as empirical PID response factors, and then used for prediction. For both approaches, the resulting information for individual species is used to model the overall PID response to a complex VOC mixture. In complement, laboratory experiments in the Harvard Environmental Chamber are carried out to measure the PID response to the complex molecular mixture produced by α-pinene oxidation under various conditions. The observations show that the measured PID response is 15% to 30% smaller than the PID response modeled by quantum-chemistry calculations of the photoionization cross section for the photo-oxidation experiments and 15% to 20% for the ozonolysis experiments. By comparison, the measured PID response is captured within a 95% confidence interval by the use of machine learning to model the PID response based on the empirical response factor in all experiments. Taken together, the results of this study demonstrate the application of machine learning to augment the performance of a nonselective chemical sensor. The approach can be generalized to other reactive species, oxidants, and reaction mechanisms, thus enhancing the utility and interpretability of PID measurements for studying atmospheric VOCs.
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Affiliation(s)
- Matthew
P. Stewart
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
| | - Paul E. Ohno
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
| | - Karena McKinney
- Department
of Chemistry, Colby College, Waterville, Maine 04901, United States
| | - Scot T. Martin
- School
of Engineering and Applied Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
- Department
of Earth and Planetary Sciences, Harvard
University, Cambridge, Massachusetts 02138, United States
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3
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Jin X, Fiore AM, Cohen RC. Space-Based Observations of Ozone Precursors within California Wildfire Plumes and the Impacts on Ozone-NO x-VOC Chemistry. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:14648-14660. [PMID: 37703172 DOI: 10.1021/acs.est.3c04411] [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: 09/15/2023]
Abstract
The frequency of wildfires in the western United States has escalated in recent decades. Here we examine the impacts of wildfires on ground-level ozone (O3) precursors and the O3-NOx-VOC chemistry from the source to downwind urban areas. We use satellite retrievals of nitrogen dioxide (NO2) and formaldehyde (HCHO, an indicator of VOC) from the Tropospheric Monitoring Instrument (TROPOMI) to track the evolution of O3 precursors from wildfires over California from 2018 to 2020. We improved these satellite retrievals by updating the a priori profiles and explicitly accounting for the effects of smoke aerosols. TROPOMI observations reveal that the extensive and intense fire smoke in 2020 led to an overall increase in statewide annual average HCHO and NO2 columns by 16% and 9%. The increase in the level of NO2 offsets the anthropogenic NOx emission reduction from the COVID-19 lockdown. The enhancement of NO2 within fire plumes is concentrated near the regions actively burning, whereas the enhancement of HCHO is far-reaching, extending from the source regions to urban areas downwind due to the secondary production of HCHO from longer-lived VOCs such as ethene. Consequently, a larger increase in NOx occurs in NOx-limited source regions, while a greater increase in HCHO occurs in VOC-limited urban areas, both contributing to more efficient O3 production.
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Affiliation(s)
- Xiaomeng Jin
- Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, New Jersey 08901, United States
| | - Arlene M Fiore
- Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, United States
| | - Ronald C Cohen
- Department of Chemistry, University of California Berkeley, Berkeley, California 94720, United States
- Department of Earth and Planetary Sciences, University of California Berkeley, Berkeley, California 94720, United States
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4
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Li L, Liu M, Qi Y, Zhang G, Yu R. Spatiotemporal variations and relationships of absorbing aerosol-radiation-gross primary productivity over China. ENVIRONMENTAL MONITORING AND ASSESSMENT 2022; 195:169. [PMID: 36451005 DOI: 10.1007/s10661-022-10775-5] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/20/2022] [Accepted: 11/21/2022] [Indexed: 06/17/2023]
Abstract
High-load carbonaceous and dust aerosols can significantly reduce direct radiation (DIRR), which would affect photosynthesis in terrestrial ecosystems, thereby further affecting the productivity of vegetation. Based on this, a variety of remote sensing data were used to study the spatiotemporal distributions and changing tendencies of the absorbing aerosols, CO, DIRR, and gross primary productivity (GPP) in China during 2005-2019; then, the relationships were analyzed between different types of absorbing aerosols and DIRR as well as GPP. The results showed that the annual mean absorbing aerosols index (AAI) in China during 2005-2019 was 0.39, with a slow growth rate of 0.02 year-1, and the emission of CO showed a decreasing trend with each passing year, especially in North China Plain and Sichuan Basin. Carbonaceous and dust aerosols were predominantly bounded by Hu line. The east of Hu line was the dominant area of carbonaceous aerosols, and the west of Hu line was the topographical region of dust aerosols. Near the Hu line was the dominant area of carbonaceous-dust aerosols. However, the Karamay-Urumqi-Hami area and Northeast China Plain were exceptional. During the vegetation growing season, different types of absorbing aerosols significantly negatively affected GPP. From a perspective of regional scale variation pattern, the negative effect of absorbing aerosols on vegetation productivity was the most significant in Northeast China; from the perspective of the effects of different vegetation types, the negative effect of absorbing aerosols on grasslands was greater than that of woodlands; from the perspective of the composition characteristics of aerosols, the negative effect of dust aerosols on GPP was greater than that of carbonaceous aerosols.
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Affiliation(s)
- Liang Li
- College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China
| | - Minxia Liu
- College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China.
| | - Yuhan Qi
- College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China
| | - Guojuan Zhang
- College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China
| | - Ruixin Yu
- College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China
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5
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Role of space station instruments for improving tropical carbon flux estimates using atmospheric data. NPJ Microgravity 2022; 8:51. [PMID: 36404345 PMCID: PMC9676185 DOI: 10.1038/s41526-022-00231-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/10/2022] [Accepted: 10/03/2022] [Indexed: 11/21/2022] Open
Abstract
The tropics is the nexus for many of the remaining gaps in our knowledge of environmental science, including the carbon cycle and atmospheric chemistry, with dire consequences for our ability to describe the Earth system response to a warming world. Difficulties associated with accessibility, coordinated funding models and economic instabilities preclude the establishment of a dense pan-tropical ground-based atmospheric measurement network that would otherwise help to describe the evolving state of tropical ecosystems and the associated biosphere-atmosphere fluxes on decadal timescales. The growing number of relevant sensors aboard sun-synchronous polar orbiters provide invaluable information over the remote tropics, but a large fraction of the data collected along their orbits is from higher latitudes. The International Space Station (ISS), which is in a low-inclination, precessing orbit, has already demonstrated value as a proving ground for Earth observing atmospheric sensors and as a testbed for new technology. Because low-inclination orbits spend more time collecting data over the tropics, we argue that the ISS and its successors, offer key opportunities to host new Earth-observing atmospheric sensors that can lead to a step change in our understanding of tropical carbon fluxes.
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6
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Fawole OG, Yusuf N, Sunmonu LA, Obafaye A, Audu DK, Onuorah L, Olusegun CF, Deme A, Senghor H. Impacts of COVID-19 Restrictions on Regional and Local Air Quality Across Selected West African Cities. GEOHEALTH 2022; 6:e2022GH000597. [PMID: 36248060 PMCID: PMC9538168 DOI: 10.1029/2022gh000597] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 01/27/2022] [Revised: 04/27/2022] [Accepted: 08/10/2022] [Indexed: 06/16/2023]
Abstract
The emergence of COVID-19 brought with it panic and a sense of urgency causing governments to impose strict restrictions on human activities and vehicular movements. With anthropogenic emissions, especially waste management (domestic and municipal), traffic, and industrial activities, said to be a significant contributor to ambient air pollution, this study assessed the impacts of the imposed restrictions on the concentrations and size distribution of atmospheric aerosols and concentration of gaseous pollutants over West African subregion and seven major COVID-19 epicenters in the subregion. Satellite retrievals and reanalysis data sets were used to study the impact of the restrictions on Aerosol Optical Depth (AOD) and atmospheric concentrations NO2, SO2, CO, and O3. The anomalies were computed for 2020 relative to 2017-2019 (the reference years). In 2020 relative to the reference years, for area-averaged AOD levels, there was a consequential mean percentage change between -6.7% ± 21.0% and 19.2% ± 27.9% in the epicenters and -10.1% ± 15.4% over the subregion. The levels of NO2 and SO2 also reduced substantially at the epicenters, especially during the periods when the restrictions were highly enforced. However, the atmospheric levels of CO and ozone increased slightly in 2020 compared to the reference years. This study shows that "a one cap fits all" policy cannot reduced the level of air pollutants and that traffic and industrial processes are not the predominant sources of CO in major cities in the subregion.
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Affiliation(s)
- Olusegun G. Fawole
- School of the Environment, Geography and GeosciencesUniversity of PortsmouthPortsmouthUK
- Department of Physics and Engineering PhysicsObafemi Awolowo UniversityIle‐IfeNigeria
| | - Najib Yusuf
- Centre for Atmospheric Research (CAR)National Space Research and Development AgencyKogi State UniversityAnyigba CampusAbujaNigeria
| | - Lukman A. Sunmonu
- Department of Physics and Engineering PhysicsObafemi Awolowo UniversityIle‐IfeNigeria
| | - Aderonke Obafaye
- Centre for Atmospheric Research (CAR)National Space Research and Development AgencyKogi State UniversityAnyigba CampusAbujaNigeria
| | - Dauda K. Audu
- Centre for Atmospheric Research (CAR)National Space Research and Development AgencyKogi State UniversityAnyigba CampusAbujaNigeria
| | - Loretta Onuorah
- Department of Physical and GeosciencesGodfrey Okoye UniversityEnuguNigeria
| | - Christiana F. Olusegun
- Centre for Atmospheric Research (CAR)National Space Research and Development AgencyKogi State UniversityAnyigba CampusAbujaNigeria
| | - Abdoulaye Deme
- UFR Sciences Appliquees et Technologie (SAT)Universite Gaston BergerSaint‐LouisSenegal
| | - Habib Senghor
- Senegalese National Agency of Civil Aviation and Meteorology (ANACIM)DakarSenegal
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7
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Ambient Formaldehyde over the United States from Ground-Based (AQS) and Satellite (OMI) Observations. REMOTE SENSING 2022. [DOI: 10.3390/rs14092191] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/17/2022]
Abstract
This study evaluates formaldehyde (HCHO) over the U.S. from 2006 to 2015 by comparing ground monitor data from the Air Quality System (AQS) and a satellite retrieval from the Ozone Monitoring Instrument (OMI). Our comparison focuses on the utility of satellite data to inform patterns, trends, and processes of ground-based HCHO across the U.S. We find that cities with higher levels of biogenic volatile organic compound (BVOC) emissions, including primary HCHO, exhibit larger HCHO diurnal amplitudes in surface observations. These differences in hour-to-hour variability in surface HCHO suggests that satellite agreement with ground-based data may depend on the distribution of emission sources. On a seasonal basis, OMI exhibits the highest correlation with AQS in summer and the lowest correlation in winter. The ratios of HCHO in summer versus other seasons show pronounced seasonal variability in OMI, likely due to seasonal changes in the vertical HCHO distribution. The seasonal variability in HCHO from satellite is more pronounced than at the surface, with seasonal variability 20–100% larger in satellite than surface observations. The seasonal variability also has a latitude dependency, with more variability in higher latitude regions. OMI agrees with AQS on the interannual variability in certain periods, whereas AQS and OMI do not show a consistent decadal trend. This is possibly due to a rather large interannual variability in HCHO, which makes the small decadal drift less significant. Temperature also explains part of the interannual variabilities. Small temperature variations in the western U.S. are reflected with more quiescent HCHO interannual variability in that region. The decrease in summertime HCHO in the southeast U.S. could also be partially explained by a small and negative trend in local temperatures.
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8
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Impact of Drought on Isoprene Fluxes Assessed Using Field Data, Satellite-Based GLEAM Soil Moisture and HCHO Observations from OMI. REMOTE SENSING 2022. [DOI: 10.3390/rs14092021] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 02/07/2023]
Abstract
Biogenic volatile organic compounds (BVOCs), primarily emitted by terrestrial vegetation, are highly reactive and have large effects on the oxidizing potential of the troposphere, air quality and climate. In terms of global emissions, isoprene is the most important BVOC. Droughts bring about changes in the surface emission of biogenic hydrocarbons mainly because plants suffer water stress. Past studies report that the current parameterization in the state-of-the-art Model of Emissions of Gases and Aerosols from Nature (MEGAN) v2.1, which is a function of the soil water content and the permanent wilting point, fails at representing the strong reduction in isoprene emissions observed in field measurements conducted during a severe drought. Since the current algorithm was originally developed based on potted plants, in this study, we update the parameterization in the light of recent ecosystem-scale measurements of isoprene conducted during natural droughts in the central U.S. at the Missouri Ozarks AmeriFlux (MOFLUX) site. The updated parameterization results in stronger reductions in isoprene emissions. Evaluation using satellite formaldehyde (HCHO), a proxy for BVOC emissions, and a chemical-transport model, shows that the adjusted parameterization provides a better agreement between the modelled and observed HCHO temporal variability at local and regional scales in 2011–2012, even if it worsens the model agreement in a global, long-term evaluation. We discuss the limitations of the current parameterization, a function of highly uncertain soil properties such as porosity.
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9
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Choi J, Henze DK, Cao H, Nowlan CR, González Abad G, Kwon H, Lee H, Oak YJ, Park RJ, Bates KH, Maasakkers JD, Wisthaler A, Weinheimer AJ. An Inversion Framework for Optimizing Non-Methane VOC Emissions Using Remote Sensing and Airborne Observations in Northeast Asia During the KORUS-AQ Field Campaign. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2022; 127:e2021JD035844. [PMID: 35865789 PMCID: PMC9285978 DOI: 10.1029/2021jd035844] [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: 09/10/2021] [Revised: 02/09/2022] [Accepted: 03/25/2022] [Indexed: 06/15/2023]
Abstract
We aim to reduce uncertainties in CH2O and other volatile organic carbon (VOC) emissions through assimilation of remote sensing data. We first update a three-dimensional (3D) chemical transport model, GEOS-Chem with the KORUSv5 anthropogenic emission inventory and inclusion of chemistry for aromatics and C2H4, leading to modest improvements in simulation of CH2O (normalized mean bias (NMB): -0.57 to -0.51) and O3 (NMB: -0.25 to -0.19) compared against DC-8 aircraft measurements during KORUS-AQ; the mixing ratio of most VOC species are still underestimated. We next constrain VOC emissions using CH2O observations from two satellites (OMI and OMPS) and the DC-8 aircraft during KORUS-AQ. To utilize data from multiple platforms in a consistent manner, we develop a two-step Hybrid Iterative Finite Difference Mass Balance and four-dimensional variational inversion system (Hybrid IFDMB-4DVar). The total VOC emissions throughout the domain increase by 47%. The a posteriori simulation reduces the low biases of simulated CH2O (NMB: -0.51 to -0.15), O3 (NMB: -0.19 to -0.06), and VOCs. Alterations to the VOC speciation from the 4D-Var inversion include increases of biogenic isoprene emissions in Korea and anthropogenic emissions in Eastern China. We find that the IFDMB method alone is adequate for reducing the low biases of VOCs in general; however, 4D-Var provides additional refinement of high-resolution emissions and their speciation. Defining reasonable emission errors and choosing optimal regularization parameters are crucial parts of the inversion system. Our new hybrid inversion framework can be applied for future air quality campaigns, maximizing the value of integrating measurements from current and upcoming geostationary satellite instruments.
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Affiliation(s)
- Jinkyul Choi
- Environmental Engineering ProgramUniversity of ColoradoBoulderCOUSA
| | - Daven K. Henze
- Department of Mechanical EngineeringUniversity of ColoradoBoulderCOUSA
| | - Hansen Cao
- Department of Mechanical EngineeringUniversity of ColoradoBoulderCOUSA
| | | | | | | | - Hyung‐Min Lee
- Department of Environmental Science and EngineeringEwha Womans UniversitySeoulSouth Korea
| | - Yujin J. Oak
- School of Earth and Environmental SciencesSeoul National UniversitySeoulSouth Korea
| | - Rokjin J. Park
- School of Earth and Environmental SciencesSeoul National UniversitySeoulSouth Korea
| | - Kelvin H. Bates
- School of Engineering and Applied SciencesHarvard UniversityCambridgeMAUSA
| | | | - Armin Wisthaler
- Institute for Ion Physics and Applied PhysicsUniversity of InnsbruckInnsbruckAustria
- Department of ChemistryUniversity of OsloOsloNorway
| | - Andrew J. Weinheimer
- Atmospheric Chemistry Observations and Modeling LaboratoryNational Center for Atmospheric ResearchBoulderCOUSA
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10
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Vohra K, Marais EA, Bloss WJ, Schwartz J, Mickley LJ, Van Damme M, Clarisse L, Coheur PF. Rapid rise in premature mortality due to anthropogenic air pollution in fast-growing tropical cities from 2005 to 2018. SCIENCE ADVANCES 2022; 8:eabm4435. [PMID: 35394832 PMCID: PMC8993110 DOI: 10.1126/sciadv.abm4435] [Citation(s) in RCA: 11] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/17/2021] [Accepted: 02/18/2022] [Indexed: 05/19/2023]
Abstract
Tropical cities are experiencing rapid growth but lack routine air pollution monitoring to develop prescient air quality policies. Here, we conduct targeted sampling of recent (2000s to 2010s) observations of air pollutants from space-based instruments over 46 fast-growing tropical cities. We quantify significant annual increases in nitrogen dioxide (NO2) (1 to 14%), ammonia (2 to 12%), and reactive volatile organic compounds (1 to 11%) in most cities, driven almost exclusively by emerging anthropogenic sources rather than traditional biomass burning. We estimate annual increases in urban population exposure to air pollutants of 1 to 18% for fine particles (PM2.5) and 2 to 23% for NO2 from 2005 to 2018 and attribute 180,000 (95% confidence interval: -230,000 to 590,000) additional premature deaths in 2018 (62% increase relative to 2005) to this increase in exposure. These cities are predicted to reach populations of up to 80 million people by 2100, so regulatory action targeting emerging anthropogenic sources is urgently needed.
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Affiliation(s)
- Karn Vohra
- School of Geography, Earth, and Environmental Sciences, University of Birmingham, Birmingham, UK
- Department of Geography, University College London, London, UK
- Corresponding author. (E.A.M.); (K.V.)
| | - Eloise A. Marais
- Department of Geography, University College London, London, UK
- Corresponding author. (E.A.M.); (K.V.)
| | - William J. Bloss
- School of Geography, Earth, and Environmental Sciences, University of Birmingham, Birmingham, UK
| | - Joel Schwartz
- Department of Environmental Health, Harvard T.H. Chan School of Public Health, Harvard University, Boston, MA, USA
| | - Loretta J. Mickley
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Martin Van Damme
- Université libre de Bruxelles (ULB), Spectroscopy, Quantum Chemistry and Atmospheric Remote Sensing (SQUARES), Brussels, Belgium
| | - Lieven Clarisse
- Université libre de Bruxelles (ULB), Spectroscopy, Quantum Chemistry and Atmospheric Remote Sensing (SQUARES), Brussels, Belgium
| | - Pierre-F. Coheur
- Université libre de Bruxelles (ULB), Spectroscopy, Quantum Chemistry and Atmospheric Remote Sensing (SQUARES), Brussels, Belgium
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11
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Morfopoulos C, Müller J, Stavrakou T, Bauwens M, De Smedt I, Friedlingstein P, Prentice IC, Regnier P. Vegetation responses to climate extremes recorded by remotely sensed atmospheric formaldehyde. GLOBAL CHANGE BIOLOGY 2022; 28:1809-1822. [PMID: 34510653 PMCID: PMC9290652 DOI: 10.1111/gcb.15880] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/25/2021] [Accepted: 07/13/2021] [Indexed: 06/01/2023]
Abstract
Accurate monitoring of vegetation stress is required for better modelling and forecasting of primary production, in a world where heatwaves and droughts are expected to become increasingly prevalent. Variability in formaldehyde (HCHO) concentrations in the troposphere is dominated by local emissions of short-lived biogenic (BVOC) and pyrogenic volatile organic compounds. BVOCs are emitted by plants in a rapid protective response to abiotic stress, mediated by the energetic status of leaves (the excess of reducing power when photosynthetic light and dark reactions are decoupled, as occurs when stomata close in response to water stress). Emissions also increase exponentially with leaf temperature. New analytical methods for the detection of spatiotemporally contiguous extremes in remote-sensing data are applied here to satellite-derived atmospheric HCHO columns. BVOC emissions are shown to play a central role in the formation of the largest positive HCHO anomalies. Although vegetation stress can be captured by various remotely sensed quantities, spaceborne HCHO emerges as the most consistent recorder of vegetation responses to the largest climate extremes, especially in forested regions.
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Affiliation(s)
- Catherine Morfopoulos
- Department of Life SciencesImperial College LondonSilwood ParkUK
- Department of Geoscience, Environment & Society‐BGEOSYSUniversité Libre de BruxellesBrusselsBelgium
| | | | | | - Maite Bauwens
- Royal Belgian Institute for Space AeronomyBrusselsBelgium
| | | | - Pierre Friedlingstein
- College of Engineering, Mathematics and Physical SciencesUniversity of ExeterExeterUK
| | - Iain Colin Prentice
- Department of Life SciencesImperial College LondonSilwood ParkUK
- Ministry of Education Key Laboratory for Earth System ModelingDepartment of Earth System ScienceTsinghua UniversityBeijingChina
- Department of Biological SciencesMacquarie UniversityNorth RydeNew South WalesAustralia
| | - Pierre Regnier
- Department of Geoscience, Environment & Society‐BGEOSYSUniversité Libre de BruxellesBrusselsBelgium
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12
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Souri AH, Chance K, Bak J, Nowlan CR, Abad GG, Jung Y, Wong DC, Mao J, Liu X. Unraveling pathways of elevated ozone induced by the 2020 lockdown in Europe by an observationally constrained regional model using TROPOMI. ATMOSPHERIC CHEMISTRY AND PHYSICS 2021; 21:1-19. [PMID: 34987561 PMCID: PMC8721815 DOI: 10.5194/acp-21-18227-2021] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Indexed: 06/14/2023]
Abstract
Questions about how emissions are changing during the COVID-19 lockdown periods cannot be answered by observations of atmospheric trace gas concentrations alone, in part due to simultaneous changes in atmospheric transport, emissions, dynamics, photochemistry, and chemical feedback. A chemical transport model simulation benefiting from a multi-species inversion framework using well-characterized observations should differentiate those influences enabling to closely examine changes in emissions. Accordingly, we jointly constrain NO x and VOC emissions using well-characterized TROPOspheric Monitoring Instrument (TROPOMI) HCHO and NO2 columns during the months of March, April, and May 2020 (lockdown) and 2019 (baseline). We observe a noticeable decline in the magnitude of NO x emissions in March 2020 (14 %-31 %) in several major cities including Paris, London, Madrid, and Milan, expanding further to Rome, Brussels, Frankfurt, Warsaw, Belgrade, Kyiv, and Moscow (34 %-51 %) in April. However, NO x emissions remain at somewhat similar values or even higher in some portions of the UK, Poland, and Moscow in March 2020 compared to the baseline, possibly due to the timeline of restrictions. Comparisons against surface monitoring stations indicate that the constrained model underrepresents the reduction in surface NO2. This underrepresentation correlates with the TROPOMI frequency impacted by cloudiness. During the month of April, when ample TROPOMI samples are present, the surface NO2 reductions occurring in polluted areas are described fairly well by the model (model: -21 ± 17 %, observation: -29 ± 21 %). The observational constraint on VOC emissions is found to be generally weak except for lower latitudes. Results support an increase in surface ozone during the lockdown. In April, the constrained model features a reasonable agreement with maximum daily 8 h average (MDA8) ozone changes observed at the surface (r = 0.43), specifically over central Europe where ozone enhancements prevail (model: +3.73 ± 3.94 %, + 1.79 ppbv, observation: +7.35 ± 11.27 %, +3.76 ppbv). The model suggests that physical processes (dry deposition, advection, and diffusion) decrease MDA8 surface ozone in the same month on average by -4.83 ppbv, while ozone production rates dampened by largely negative J NO 2 [ NO 2 ] - k NO + O 3 [ NO ] [ O 3 ] become less negative, leading ozone to increase by +5.89 ppbv. Experiments involving fixed anthropogenic emissions suggest that meteorology contributes to 42 % enhancement in MDA8 surface ozone over the same region with the remaining part (58 %) coming from changes in anthropogenic emissions. Results illustrate the capability of satellite data of major ozone precursors to help atmospheric models capture ozone changes induced by abrupt emission anomalies.
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Affiliation(s)
- Amir H. Souri
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Kelly Chance
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Juseon Bak
- Institute of Environmental Studies, Pusan National University, Busan, South Korea
| | - Caroline R. Nowlan
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Gonzalo González Abad
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Yeonjin Jung
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - David C. Wong
- US Environmental Protection Agency, Center for Environmental Measurement & Modeling, Research Triangle Park, NC, USA
| | - Jingqiu Mao
- Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA
- Department of Chemistry and Biochemistry, University of Alaska Fairbanks, Fairbanks, AK, USA
| | - Xiong Liu
- Atomic and Molecular Physics (AMP) Division, Harvard–Smithsonian Center for Astrophysics, Cambridge, MA, USA
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13
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Yang W, Cao J, Wu Y, Kong F, Li L. Review on plant terpenoid emissions worldwide and in China. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 787:147454. [PMID: 34000546 DOI: 10.1016/j.scitotenv.2021.147454] [Citation(s) in RCA: 18] [Impact Index Per Article: 6.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/10/2021] [Revised: 04/26/2021] [Accepted: 04/26/2021] [Indexed: 05/21/2023]
Abstract
Biogenic volatile organic compounds (BVOCs), particularly terpenoids, can significantly drive the formation of ozone (O3) and secondary organic aerosols (SOA) in the atmosphere, as well as directly or indirectly affect global climate change. Understanding their emission mechanisms and the current progress in emission measurements and estimations are essential for the accurate determination of emission characteristics, as well as for evaluating their roles in atmospheric chemistry and climate change. This review summarizes the mechanisms of terpenoid synthesis and release, biotic and abiotic factors affecting their emissions, development of emission observation techniques, and emission estimations from hundreds of published papers. We provide a review of the main observations and estimations in China, which contributes a significant proportion to the total global BVOC emissions. The review suggests the need for further research on the comprehensive effects of environmental factors on terpenoid emissions, especially soil moisture and nitrogen content, which should be quantified in emission models to improve the accuracy of estimation. In China, it is necessary to conduct more accurate measurements for local plants in different regions using the dynamic enclosure technique to establish an accurate local emission rate database for dominant tree species. This will help improve the accuracy of both national and global emission inventories. This review provides a comprehensive understanding of terpenoid emissions as well as prospects for detailed research to accurately describe terpenoid emission characteristics worldwide and in China.
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Affiliation(s)
- Weizhen Yang
- College of Environmental Sciences and Engineering, Qingdao University, Qingdao 266071, China
| | - Jing Cao
- College of Environmental Sciences and Engineering, Qingdao University, Qingdao 266071, China
| | - Yan Wu
- School of Environmental Science and Engineering, Shandong University, Qingdao 266237, China
| | - Fanlong Kong
- College of Environmental Sciences and Engineering, Qingdao University, Qingdao 266071, China.
| | - Lingyu Li
- College of Environmental Sciences and Engineering, Qingdao University, Qingdao 266071, China.
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Atmospheric Impacts of COVID-19 on NOx and VOC Levels over China Based on TROPOMI and IASI Satellite Data and Modeling. ATMOSPHERE 2021. [DOI: 10.3390/atmos12080946] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
China was the first country to undergo large-scale lockdowns in response to the pandemic in early 2020 and a progressive return to normalization after April 2020. Spaceborne observations of atmospheric nitrogen dioxide (NO2) and oxygenated volatile organic compounds (OVOCs), including formaldehyde (HCHO), glyoxal (CHOCHO), and peroxyacetyl nitrate (PAN), reveal important changes over China in 2020, relative to 2019, in response to the pandemic-induced shutdown and the subsequent drop in pollutant emissions. In February, at the peak of the shutdown, the observed declines in OVOC levels were generally weaker (less than 20%) compared to the observed NO2 reductions (−40%). In May 2020, the observations reveal moderate decreases in NO2 (−15%) and PAN (−21%), small changes in CHOCHO (−3%) and HCHO (6%). Model simulations using the regional model MAGRITTEv1.1 with anthropogenic emissions accounting for the reductions due to the pandemic explain to a large extent the observed changes in lockdown-affected regions. The model results suggest that meteorological variability accounts for a minor but non-negligible part (~−5%) of the observed changes for NO2, whereas it is negligible for CHOCHO but plays a more substantial role for HCHO and PAN, especially in May. The interannual variability of biogenic and biomass burning emissions also contribute to the observed variations, explaining e.g., the important column increases of NO2 and OVOCs in February 2020, relative to 2019. These changes are well captured by the model simulations.
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15
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Harkey M, Holloway T, Kim EJ, Baker KR, Henderson B. Satellite Formaldehyde to Support Model Evaluation. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2021; 126:10.1029/2020jd032881. [PMID: 34381662 PMCID: PMC8353957 DOI: 10.1029/2020jd032881] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/08/2020] [Accepted: 12/16/2020] [Indexed: 06/13/2023]
Abstract
Formaldehyde (HCHO), a known carcinogen classified as a hazardous pollutant by the United States Environmental Protection Agency (U.S. EPA), is measured through monitoring networks across the U.S. Since these data are limited in spatial and temporal extent, model simulations from the U.S. EPA Community Multiscale Air Quality (CMAQ) model are used to estimate ambient HCHO exposure for the EPA National Air Toxics Assessment (NATA). Here, we employ satellite HCHO retrievals from the Ozone Monitoring Instrument (OMI)-the NASA retrieval developed by the Smithsonian Astrophysical Observatory (SAO), and the European Union Quality Assurance for Essential Climate Variables (QA4ECV) retrieval-to evaluate three CMAQ configurations, spanning the summers of 2011 and 2016, with differing biogenic emissions inputs and chemical mechanisms. These CMAQ configurations capture the general spatial and temporal behavior of both satellite retrievals, but underestimate column HCHO, particularly in the western U.S. In the southeastern U.S., the comparison with OMI HCHO highlights differences in modeled meteorology and biogenic emissions even with differences in satellite retrievals. All CMAQ configurations show low daily correlations with OMI HCHO (r = 0.26 - 0.38), however, we find higher monthly correlations (r = 0.52 - 0.73), and the models correlate best with the OMI-QA4ECV product. Compared to surface observations, we find improved agreement over a 24-hour period compared to afternoon-only, suggesting daily HCHO amounts are captured with more accuracy than afternoon amounts. This work highlights the potential for synergistic improvements in modeling and satellite retrievals to support near-surface HCHO estimates for the NATA and other applications.
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Affiliation(s)
- Monica Harkey
- Nelson Institute Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Ave, Madison WI 53726
| | - Tracey Holloway
- Nelson Institute Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Ave, Madison WI 53726
- Department of Atmospheric & Oceanic Sciences, University of Wisconsin-Madison, 1225 W Dayton Street, Madison, WI 53706
| | - Eliot J. Kim
- Nelson Institute Center for Sustainability and the Global Environment (SAGE), University of Wisconsin-Madison, 1710 University Ave, Madison WI 53726
| | - Kirk R. Baker
- U.S. Environmental Protection Agency, Research Triangle Park, NC, USA
| | - Barron Henderson
- U.S. Environmental Protection Agency, Research Triangle Park, NC, USA
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16
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Wells KC, Millet DB, Payne VH, Deventer MJ, Bates KH, de Gouw JA, Graus M, Warneke C, Wisthaler A, Fuentes JD. Satellite isoprene retrievals constrain emissions and atmospheric oxidation. Nature 2020; 585:225-233. [PMID: 32908268 PMCID: PMC7490801 DOI: 10.1038/s41586-020-2664-3] [Citation(s) in RCA: 27] [Impact Index Per Article: 6.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/17/2019] [Accepted: 07/14/2020] [Indexed: 11/09/2022]
Abstract
Isoprene is the dominant non-methane organic compound emitted to the atmosphere1-3. It drives ozone and aerosol production, modulates atmospheric oxidation and interacts with the global nitrogen cycle4-8. Isoprene emissions are highly uncertain1,9, as is the nonlinear chemistry coupling isoprene and the hydroxyl radical, OH-its primary sink10-13. Here we present global isoprene measurements taken from space using the Cross-track Infrared Sounder. Together with observations of formaldehyde, an isoprene oxidation product, these measurements provide constraints on isoprene emissions and atmospheric oxidation. We find that the isoprene-formaldehyde relationships measured from space are broadly consistent with the current understanding of isoprene-OH chemistry, with no indication of missing OH recycling at low nitrogen oxide concentrations. We analyse these datasets over four global isoprene hotspots in relation to model predictions, and present a quantification of isoprene emissions based directly on satellite measurements of isoprene itself. A major discrepancy emerges over Amazonia, where current underestimates of natural nitrogen oxide emissions bias modelled OH and hence isoprene. Over southern Africa, we find that a prominent isoprene hotspot is missing from bottom-up predictions. A multi-year analysis sheds light on interannual isoprene variability, and suggests the influence of the El Niño/Southern Oscillation.
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Affiliation(s)
- Kelley C Wells
- Department of Soil, Water, and Climate, University of Minnesota, St Paul, MN, USA
| | - Dylan B Millet
- Department of Soil, Water, and Climate, University of Minnesota, St Paul, MN, USA.
| | - Vivienne H Payne
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
| | - M Julian Deventer
- Department of Soil, Water, and Climate, University of Minnesota, St Paul, MN, USA
- Bioclimatology, University of Göttingen, Göttingen, Germany
| | - Kelvin H Bates
- School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Joost A de Gouw
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- Department of Chemistry, University of Colorado, Boulder, CO, USA
| | - Martin Graus
- Department of Atmospheric and Cryogenic Sciences, University of Innsbruck, Innsbruck, Austria
| | - Carsten Warneke
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA
- NOAA Chemical Sciences Laboratory, Boulder, CO, USA
| | - Armin Wisthaler
- Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Department of Chemistry, University of Oslo, Oslo, Norway
| | - Jose D Fuentes
- Department of Meteorology and Atmospheric Science, The Pennsylvania State University, University Park, PA, USA
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17
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Wang Y, Zhao Y, Zhang L, Zhang J, Liu Y. Modified regional biogenic VOC emissions with actual ozone stress and integrated land cover information: A case study in Yangtze River Delta, China. THE SCIENCE OF THE TOTAL ENVIRONMENT 2020; 727:138703. [PMID: 32334230 DOI: 10.1016/j.scitotenv.2020.138703] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/19/2020] [Revised: 04/12/2020] [Accepted: 04/13/2020] [Indexed: 06/11/2023]
Abstract
The biogenic volatile organic compounds (BVOCs) emissions are influenced by ambient ozone (O3) concentrations and vegetation cover. In most studies, however, the interaction between O3 and plants has not been considered and there are uncertainties in land cover input and emission factors (EFs) in BVOCs emission estimation, particularly at the regional scale. In this study, an O3 exposure-isoprene (ISOP) response function was developed using meta-analysis, and the EFs of ISOP and land cover inputs were updated by integrating local measurement and investigation data in the Yangtze River Delta (YRD) region. Five different cases were developed to explore the impacts of O3 and input variables on the BVOCs emissions using the Model of Emissions of Gases and Aerosols from Nature (MEGAN). The impacts of those variables on O3 simulation were further examined with air quality modeling. We found that the ISOP emissions were restrained in the city cluster along the Yangtze River during the growing season due to their negative feedback to O3 exposure for deciduous broadleaf forests. The estimation of BVOCs emissions strongly depended on EFs, and the global EFs underestimated the ISOP emissions in July by 37%, mostly in southern YRD. Different land cover datasets with various fractions and spatial distributions of plant function types resulted in a variation of 200-400 Gg in ISOP emissions in July across YRD. Air quality modeling indicated that BVOCs contributed 10%, 12%, and 11% to the 1-h mean, the maximum daily 1-h average, and the maximum daily 8-h average O3 concentrations, respectively, for July across the YRD region. Due to the NOx restriction, the spatial distribution of BVOCs emissions was inconsistent with that of their contribution to O3 formation. The O3 simulation was more sensitive to the changed BVOCs emissions in the area with relatively large contribution of BVOCs to O3 formation.
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Affiliation(s)
- Yutong Wang
- State Key Laboratory of Pollution Control and Resource Reuse and School of the Environment, Nanjing University, 163 Xianlin Ave., Nanjing, Jiangsu 210023, China
| | - Yu Zhao
- State Key Laboratory of Pollution Control and Resource Reuse and School of the Environment, Nanjing University, 163 Xianlin Ave., Nanjing, Jiangsu 210023, China; Jiangsu Collaborative Innovation Center of Atmospheric Environment and Equipment Technology (CICAEET), Nanjing University of Information Science and Technology, Jiangsu 210044, China.
| | - Lei Zhang
- State Key Laboratory of Pollution Control and Resource Reuse and School of the Environment, Nanjing University, 163 Xianlin Ave., Nanjing, Jiangsu 210023, China
| | - Jie Zhang
- Jiangsu Provincial Academy of Environmental Science, 176 North Jiangdong Rd., Nanjing, Jiangsu 210036, China
| | - Yang Liu
- Department of Environmental Health, Emory University, Rollins School of Public Health, Atlanta, GA 30322, United States
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18
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Jin X, Fiore A, Boersma KF, Smedt ID, Valin L. Inferring Changes in Summertime Surface Ozone-NO x-VOC Chemistry over U.S. Urban Areas from Two Decades of Satellite and Ground-Based Observations. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2020; 54:6518-6529. [PMID: 32348127 PMCID: PMC7996126 DOI: 10.1021/acs.est.9b07785] [Citation(s) in RCA: 51] [Impact Index Per Article: 12.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/21/2023]
Abstract
Urban ozone (O3) formation can be limited by NOx, VOCs, or both, complicating the design of effective O3 abatement plans. A satellite-retrieved ratio of formaldehyde to NO2 (HCHO/NO2), developed from theory and modeling, has previously been used to indicate O3 formation chemistry. Here, we connect this space-based indicator to spatiotemporal variations in O3 recorded by on-the-ground monitors over major U.S. cities. High-O3 events vary nonlinearly with OMI HCHO and NO2, and the transition from VOC-limited to NOx-limited O3 formation regimes occurs at higher HCHO/NO2 value (3 to 4) than previously determined from models, with slight intercity variations. To extend satellite records back to 1996, we develop an approach to harmonize observations from GOME and SCIAMACHY that accounts for differences in spatial resolution and overpass time. Two-decade (1996-2016) multisatellite HCHO/NO2 captures the timing and location of the transition from VOC-limited to NOx-limited O3 production regimes in major U.S. cities, which aligns with the observed long-term changes in urban-rural gradient of O3 and the reversal of O3 weekend effect. Our findings suggest promise for applying space-based HCHO/NO2 to interpret local O3 chemistry, particularly with the new-generation satellite instruments that offer finer spatial and temporal resolution.
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Affiliation(s)
- Xiaomeng Jin
- Department of Earth and Environmental Sciences, Columbia University, New York, NY, USA
- Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Arlene Fiore
- Department of Earth and Environmental Sciences, Columbia University, New York, NY, USA
- Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - K Folkert Boersma
- Royal Netherlands Meteorological Institute, De Bilt, The Netherlands
- Wageningen University, Environmental Sciences Group, Wageningen, The Netherlands
| | | | - Lukas Valin
- U.S. EPA Office of Research and Development, Research Triangle Park, NC, USA
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19
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Zhang T, Chillrud SN, Yang Q, Pitiranggon M, Ross J, Perera F, Ji J, Spira A, Breysse PN, Rodes CE, Miller R, Yan B. Characterizing peak exposure of secondhand smoke using a real-time PM 2.5 monitor. INDOOR AIR 2020; 30:98-107. [PMID: 31610044 PMCID: PMC7137634 DOI: 10.1111/ina.12611] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/28/2019] [Revised: 08/15/2019] [Accepted: 10/10/2019] [Indexed: 06/10/2023]
Abstract
Although short-duration elevated exposures (peak exposures) to pollutants may trigger adverse acute effects, epidemiological studies to understand their influence on different health effects are hampered by lack of methods for objectively identifying peaks. Secondhand smoke from cigarettes (SHS) in the residential environment can lead to peak exposures. The aim of this study was to explore whether peaks in continuous PM2.5 data can indicate SHS exposure. A total of 41 children (21 with and 20 without SHS exposure based on self-report) from 28 families in New York City (NY, USA) were recruited. Both personal and residential continuous PM2.5 monitoring were performed for five consecutive days using MicroPEM sensors (RTI International, USA). A threshold detection method based on cumulative distribution function was developed to identify peaks. When children were home, the mean accumulated peak area (APA) for peak exposures was 297 ± 325 hour*µg/m3 for children from smoking families and six times that of the APA from non-smoking families (~50 ± 54 hour*µg/m3 ). Average PM2.5 mass concentrations for SHS exposed and unexposed children were 24 ± 15 µg/m3 and 15 ± 9 µg/m3 , respectively. The average SHS exposure duration represents ~5% of total exposure time, but ~13% of children's total PM2.5 exposure dose, equivalent to an additional 2.6 µg/m3 per day. This study demonstrated the feasibility of peak analysis for quantifying SHS exposure. The developed method can be adopted more widely to support epidemiology studies on impacts of short-term exposures.
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Affiliation(s)
- Ting Zhang
- Key Laboratory of Surficial Geochemistry, Ministry of Education, Nanjing University, Nanjing, China
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Steven N. Chillrud
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Qiang Yang
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Masha Pitiranggon
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - James Ross
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Frederica Perera
- Department of Environmental Health Sciences, Mailman School of Public Health, Columbia University, New York, NY, USA
| | - Junfeng Ji
- Key Laboratory of Surficial Geochemistry, Ministry of Education, Nanjing University, Nanjing, China
| | - Avrum Spira
- Boston University-Boston Medical Center Cancer Center, Boston University School of Medicine, Boston, MA, USA
| | - Patrick N. Breysse
- Department of Environmental Health and Engineering, Johns Hopkins Bloomberg School of Public Health, Baltimore, MD, USA
| | | | - Rachel Miller
- Department of Environmental Health Sciences, Mailman School of Public Health, Columbia University, New York, NY, USA
- Department of Medicine, College of Physicians and Surgeons, Division of Pulmonary, Allergy and Critical Care of Medicine, Columbia University, New York, NY, USA
| | - Beizhan Yan
- Lamont Doherty Earth Observatory of Columbia University, Palisades, NY, USA
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20
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Chaliyakunnel S, Millet DB, Chen X. Constraining Emissions of Volatile Organic Compounds Over the Indian Subcontinent Using Space-Based Formaldehyde Measurements. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2019; 124:10525-10545. [PMID: 33614368 PMCID: PMC7894393 DOI: 10.1029/2019jd031262] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.4] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/02/2019] [Accepted: 08/26/2019] [Indexed: 06/11/2023]
Abstract
India is an air pollution mortality hot spot, but regional emissions are poorly understood. We present a high-resolution nested chemical transport model (GEOS-Chem) simulation for the Indian subcontinent and use it to interpret formaldehyde (HCHO) observations from two satellite sensors (OMI and GOME-2A) in terms of constraints on regional volatile organic compound (VOC) emissions. We find modeled biogenic VOC emissions to be overestimated by ~30-60% for most locations and seasons, and derive a best estimate biogenic flux of 16 Tg C/year subcontinent-wide for year 2009. Terrestrial vegetation provides approximately half the total VOC flux in our base-case inversions (full uncertainty range: 44-65%). This differs from prior understanding, in which biogenic emissions represent >70% of the total. Our derived anthropogenic VOC emissions increase slightly (13-16% in the base case, for a subcontinent total of 15 Tg C/year in 2009) over RETRO year 2000 values, with some larger regional discrepancies. The optimized anthropogenic emissions agree well with the more recent CEDS inventory, both subcontinent-wide (within 2%) and regionally. An exception is the Indo-Gangetic Plain, where we find an underestimate for both RETRO and CEDS. Anthropogenic emissions thus constitute 37-50% of the annual regional VOC source in our base-case inversions and exceed biogenic emissions over the Indo-Gangetic Plain, West India, and South India, and over the entire subcontinent during winter and post-monsoon. Fires are a minor fraction (<7%) of the total regional VOC source in the prior and optimized model. However, evidence suggests that VOC emissions in the fire inventory used here (GFEDv4) are too low over the Indian subcontinent.
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Affiliation(s)
- Sreelekha Chaliyakunnel
- Department of Soil, Water, and Climate, University of Minnesota, Twin Cities, St. Paul, MN, USA
| | - Dylan B Millet
- Department of Soil, Water, and Climate, University of Minnesota, Twin Cities, St. Paul, MN, USA
| | - Xin Chen
- Department of Soil, Water, and Climate, University of Minnesota, Twin Cities, St. Paul, MN, USA
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21
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Xing Y, Li H, Huang L, Wu H, Shen H, Chen Z. The production of formaldehyde and hydroxyacetone in methacrolein photooxidation: New insights into mechanism and effects of water vapor. J Environ Sci (China) 2018; 66:1-11. [PMID: 29628075 DOI: 10.1016/j.jes.2017.05.037] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.2] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/28/2017] [Revised: 05/19/2017] [Accepted: 05/26/2017] [Indexed: 06/08/2023]
Abstract
Methacrolein (MACR) is an abundant multifunctional carbonyl compound with high reactivity in the atmosphere. In this study, we investigated the hydroxyl radical initiated oxidation of MACR at various NO/MACR ratios (0 to 4.04) and relative humidities (<3% to 80%) using a flow tube. Meanwhile, a box model based on the Master Chemical Mechanism was performed to test our current understanding of the mechanism. In contrast to the reasonable predictions for hydroxyacetone production, the modeled yields of formaldehyde (HCHO) were twice higher than the experimental results. The discrepancy was ascribed to the existence of unconsidered non-HCHO forming channels in the chemistry of CH3C(CH2)OO, which account for approx. 50%. In addition, the production of hydroxyacetone and HCHO were affected by water vapor as well as the initial NO/MACR ratio. The yields of HCHO were higher under humid conditions than that under dry condition. The yields of hydroxyacetone were higher under humid conditions at low-NOx level, while lower at high-NOx level. The reasonable explanation for the lower hydroxyacetone yield under humid conditions at high-NOx level is that water vapor promotes the production of methacrolein nitrate in the reaction of HOCH2C(CH3)(OO)CHO with NO due to the peroxy radical-water complex formation, which was evidenced by calculational results. And the minimum equilibrium constant of this water complex formation was estimated to be 1.89×10-18cm3/molecule. These results provide new insights into the MACR oxidation mechanism and the effects of water vapor.
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Affiliation(s)
- Yanan Xing
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China.
| | - Huan Li
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Liubin Huang
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Huihui Wu
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Hengqing Shen
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China
| | - Zhongming Chen
- State Key Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China.
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22
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Liu R, Feng T, Wang S, Shi C, Guo Y, Nan J, Deng Y, Zhou B. OMI satellite observed formaldehyde column from 2006 to 2015 over Xishuangbanna, southwest China, and validation using ground based zenith-sky DOAS. THE SCIENCE OF THE TOTAL ENVIRONMENT 2018; 613-614:168-175. [PMID: 28917166 DOI: 10.1016/j.scitotenv.2017.08.210] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/26/2017] [Revised: 07/24/2017] [Accepted: 08/20/2017] [Indexed: 06/07/2023]
Abstract
Formaldehyde (HCHO) provides a proxy to reveal the isoprene and biogenic volatile organic compounds emission which plays important roles in atmospheric chemical process and climate change. The ground-based observation with zenith-sky DOAS is carried out in order to validate the HCHO columns from OMI. It has a good correlation of 0.71678 between the HCHO columns from two sources. Then we use the OMI HCHO columns from January 2006 to December 2015 to indicate the interannual variation and spatial distribution in Xishuangbanna. The HCHO concentration peaks appeared in March or April for each year significantly corresponding to the intensive fire counts at the same time, which illustrate that the high HCHO columns are strongly influenced by the biomass burning in spring. Temperature and precipitation are also the important influence factors in the seasonal variation when there is nearly no biomass burning. The spatial patterns over the past ten years strengthen the deduction from the temporal variation and show the relationship with land cover and land use, elevation and population density. It is concluded that the biogenic activity plays a role in controlling the background level of HCHO in Xishuangbanna, while biomass burning is the main driving force of high HCHO concentration. And forests are greater contributor to HCHO rather than rubber trees which cover over 20% of the land in the region. Moreover, uncertainties from HCHO slant column retrieval and AMFs calculation are discussed in detail.
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Affiliation(s)
- Rui Liu
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP(3)), Department of Environmental Science & Engineering, Fudan University, Shanghai 200433, China; School of Resource and Environment, Yunnan University, Yunnan 650000, China
| | - Tao Feng
- School of Information Science, Yunnan University of Finance and Economics, Yunnan 650000, China
| | - Shanshan Wang
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP(3)), Department of Environmental Science & Engineering, Fudan University, Shanghai 200433, China.
| | - Chanzhen Shi
- Shanghai Institute of Measurement Testing Technology, Shanghai 200233, China
| | - Yanlin Guo
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP(3)), Department of Environmental Science & Engineering, Fudan University, Shanghai 200433, China
| | - Jialiang Nan
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP(3)), Department of Environmental Science & Engineering, Fudan University, Shanghai 200433, China
| | - Yun Deng
- Xishuangbanna Tropical Botanical Garden of Chinese Academy of Sciences, Yunnan 666100, China
| | - Bin Zhou
- Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP(3)), Department of Environmental Science & Engineering, Fudan University, Shanghai 200433, China; Fudan Tyndall Centre, Fudan University, Shanghai 200433, China.
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23
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Spinei E, Whitehill A, Fried A, Tiefengraber M, Knepp TN, Herndon S, Herman JR, Müller M, Abuhassan N, Cede A, Richter D, Walega J, Crawford J, Szykman J, Valin L, Williams DJ, Long R, Swap RJ, Lee Y, Nowak N, Poche B. The first evaluation of formaldehyde column observations by improved Pandora spectrometers during the KORUS-AQ field study. ATMOSPHERIC CHEMISTRY AND PHYSICS 2018; 11:4943-4961. [PMID: 33424951 PMCID: PMC7788067 DOI: 10.5194/amt-11-4943-2018] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/06/2023]
Abstract
The Korea-United States Air Quality Study (KORUS-AQ) conducted during May-June 2016 offered the first opportunity to evaluate direct-sun observations of formaldehyde (HCHO) total column densities with improved Pandora spectrometer instruments. The measurements highlighted in this work were conducted both in the Seoul megacity area at the Olympic Park site (37.5232° N, 27.1260° E; 26 ma.s.l.) and at a nearby rural site downwind of the city at the Mount Taehwa research forest site (37.3123° N, 127.3106° E; 160ma.s.l.). Evaluation of these measurements was made possible by concurrent ground-based in situ observations of HCHO at both sites as well as overflight by the NASA DC-8 research aircraft. The flights provided in situ measurements of HCHO to characterize its vertical distribution in the lower troposphere (0-5km). Diurnal variation in HCHO total column densities followed the same pattern at both sites, with the minimum daily values typically observed between 6:00 and 7:00 local time, gradually increasing to a maximum between 13:00 and 17:00 before decreasing into the evening. Pandora vertical column densities were compared with those derived from the DC-8 HCHO in situ measured profiles augmented with in situ surface concentrations below the lowest altitude of the DC-8 in proximity to the ground sites. A comparison between 49 column densities measured by Pandora vs. aircraft-integrated in situ data showed that Pandora values were larger by 16% with a constant offset of 0.22DU (Dobson units; R 2 = 0.68). Pandora HCHO columns were also compared with columns calculated from the surface in situ measurements over Olympic Park by assuming a well-mixed lower atmosphere up to a ceilometer-measured mixed-layer height (MLH) and various assumptions about the small residual HCHO amounts in the free troposphere up to the tropopause. The best comparison (slope = 1.03±0.03; intercept = 0.29±0.02DU; and R 2 = 0.78±0.02) was achieved assuming equal mixing within ceilometer-measured MLH combined with an exponential profile shape. These results suggest that diurnal changes in HCHO surface concentrations can be reasonably estimated from the Pandora total column and information on the mixed-layer height. More work is needed to understand the bias in the intercept and the slope relative to columns derived from the in situ aircraft and surface measurements.
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Affiliation(s)
- Elena Spinei
- NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
- Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA
| | | | - Alan Fried
- Institute of Arctic and Alpine Research (INSTAAR) at the University of Colorado, Boulder, C0 80303, USA
| | - Martin Tiefengraber
- LuftBlick, Kreith 39A, 6162 Mutters, Austria
- Institue of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innsbruck, Austria
| | - Travis N. Knepp
- NASA Langley Research Center, Hampton, VA 23681, USA
- Science Systems and Applications, Inc., Hampton, VA 23681, USA
| | | | - Jay R. Herman
- NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
- University of Maryland Baltimore County, Baltimore, MD, USA
| | - Moritz Müller
- LuftBlick, Kreith 39A, 6162 Mutters, Austria
- Institue of Atmospheric and Cryospheric Sciences, University of Innsbruck, Innsbruck, Austria
| | - Nader Abuhassan
- NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
- University of Maryland Baltimore County, Baltimore, MD, USA
| | - Alexander Cede
- NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
- LuftBlick, Kreith 39A, 6162 Mutters, Austria
| | - Dirk Richter
- Institute of Arctic and Alpine Research (INSTAAR) at the University of Colorado, Boulder, C0 80303, USA
| | - James Walega
- Institute of Arctic and Alpine Research (INSTAAR) at the University of Colorado, Boulder, C0 80303, USA
| | | | - James Szykman
- US EPA, Research Triangle Park, Durham, NC 27709, USA
- NASA Langley Research Center, Hampton, VA 23681, USA
| | - Lukas Valin
- US EPA, Research Triangle Park, Durham, NC 27709, USA
| | | | - Russell Long
- US EPA, Research Triangle Park, Durham, NC 27709, USA
| | - Robert J. Swap
- NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
| | - Youngjae Lee
- Korean National Institute of Environmental Research (NIER), Incheon, South Korea
| | - Nabil Nowak
- Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA
| | - Brett Poche
- Virginia Polytechnic Institute and State University, Blacksburg, VA 24061, USA
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24
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Jin X, Fiore AM, Murray LT, Valin LC, Lamsal LN, Duncan B, Boersma KF, De Smedt I, Abad GG, Chance K, Tonnesen GS. Evaluating a Space-Based Indicator of Surface Ozone-NO x -VOC Sensitivity Over Midlatitude Source Regions and Application to Decadal Trends. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2017; 122:10-461. [PMID: 29682438 PMCID: PMC5906809 DOI: 10.1002/2017jd026720] [Citation(s) in RCA: 63] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Determining effective strategies for mitigating surface ozone (O3) pollution requires knowledge of the relative ambient concentrations of its precursors, NO x , and VOCs. The space-based tropospheric column ratio of formaldehyde to NO2 (FNR) has been used as an indicator to identify NO x -limited versus NO x -saturated O3 formation regimes. Quantitative use of this indicator ratio is subject to three major uncertainties: (1) the split between NO x -limited and NO x -saturated conditions may shift in space and time, (2) the ratio of the vertically integrated column may not represent the near-surface environment, and (3) satellite products contain errors. We use the GEOS-Chem global chemical transport model to evaluate the quantitative utility of FNR observed from the Ozone Monitoring Instrument over three northern midlatitude source regions. We find that FNR in the model surface layer is a robust predictor of the simulated near-surface O3 production regime. Extending this surface-based predictor to a column-based FNR requires accounting for differences in the HCHO and NO2 vertical profiles. We compare four combinations of two OMI HCHO and NO2 retrievals with modeled FNR. The spatial and temporal correlations between the modeled and satellite-derived FNR vary with the choice of NO2 product, while the mean offset depends on the choice of HCHO product. Space-based FNR indicates that the spring transition to NO x -limited regimes has shifted at least a month earlier over major cities (e.g., New York, London, and Seoul) between 2005 and 2015. This increase in NO x sensitivity implies that NO x emission controls will improve O3 air quality more now than it would have a decade ago.
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Affiliation(s)
- Xiaomeng Jin
- Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Arlene M Fiore
- Department of Earth and Environmental Sciences, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
| | - Lee T Murray
- Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY, USA
| | - Lukas C Valin
- U.S. EPA Office of Research and Development, Research Triangle Park, Durham, NC, USA
| | - Lok N Lamsal
- NASA Goddard Space Flight Center, Greenbelt, MD, USA
- Goddard Earth Sciences Technology and Research, Universities Space Research Association, Columbia, MD, USA
| | - Bryan Duncan
- NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - K Folkert Boersma
- Royal Netherlands Meteorological Institute, De Bilt, Netherlands
- Wageningen University, Meteorology and Air Quality Group, Wageningen, Netherlands
| | | | | | - Kelly Chance
- Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Gail S Tonnesen
- United States Environmental Protection Agency, Denver, CO, USA
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25
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Zhu L, Jacob DJ, Keutsch FN, Mickley LJ, Scheffe R, Strum M, González Abad G, Chance K, Yang K, Rappenglück B, Millet DB, Baasandorj M, Jaeglé L, Shah V. Formaldehyde (HCHO) As a Hazardous Air Pollutant: Mapping Surface Air Concentrations from Satellite and Inferring Cancer Risks in the United States. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2017; 51:5650-5657. [PMID: 28441488 DOI: 10.1021/acs.est.7b01356] [Citation(s) in RCA: 59] [Impact Index Per Article: 8.4] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/05/2023]
Abstract
Formaldehyde (HCHO) is the most important carcinogen in outdoor air among the 187 hazardous air pollutants (HAPs) identified by the U.S. Environmental Protection Agency (EPA), not including ozone and particulate matter. However, surface observations of HCHO are sparse and the EPA monitoring network could be prone to positive interferences. Here we use 2005-2016 summertime HCHO column data from the OMI satellite instrument, validated with high-quality aircraft data and oversampled on a 5 × 5 km2 grid, to map surface air HCHO concentrations across the contiguous U.S. OMI-derived summertime HCHO values are converted to annual averages using the GEOS-Chem chemical transport model. Results are in good agreement with high-quality summertime observations from urban sites (-2% bias, r = 0.95) but a factor of 1.9 lower than annual means from the EPA network. We thus estimate that up to 6600-12 500 people in the U.S. will develop cancer over their lifetimes by exposure to outdoor HCHO. The main HCHO source in the U.S. is atmospheric oxidation of biogenic isoprene, but the corresponding HCHO yield decreases as the concentration of nitrogen oxides (NOx ≡ NO + NO2) decreases. A GEOS-Chem sensitivity simulation indicates that HCHO levels would decrease by 20-30% in the absence of U.S. anthropogenic NOx emissions. Thus, NOx emission controls to improve ozone air quality have a significant cobenefit in reducing HCHO-related cancer risks.
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Affiliation(s)
- Lei Zhu
- John A. Paulson School of Engineering and Applied Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
| | - Daniel J Jacob
- John A. Paulson School of Engineering and Applied Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
- Department of Earth and Planetary Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
| | - Frank N Keutsch
- John A. Paulson School of Engineering and Applied Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
- Department of Chemistry and Chemical Biology, Harvard University , Cambridge, Massachusetts 02138, United States
| | - Loretta J Mickley
- John A. Paulson School of Engineering and Applied Sciences, Harvard University , Cambridge, Massachusetts 02138, United States
| | - Richard Scheffe
- U.S. Environmental Protection Agency, Durham, North Carolina 27711, United States
| | - Madeleine Strum
- U.S. Environmental Protection Agency, Durham, North Carolina 27711, United States
| | - Gonzalo González Abad
- Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts 02138, United States
| | - Kelly Chance
- Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts 02138, United States
| | - Kai Yang
- Department of Atmospheric and Oceanic Science, University of Maryland College Park , College Park, Maryland 20740, United States
| | - Bernhard Rappenglück
- Department of Earth and Atmospheric Sciences, University of Houston , Houston, Texas 77204, United States
| | - Dylan B Millet
- Department of Soil, Water, and Climate, University of Minnesota , Minneapolis-Saint Paul, Minnesota 55108, United States
| | - Munkhbayar Baasandorj
- Department of Soil, Water, and Climate, University of Minnesota , Minneapolis-Saint Paul, Minnesota 55108, United States
| | - Lyatt Jaeglé
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98105, United States
| | - Viral Shah
- Department of Atmospheric Sciences, University of Washington , Seattle, Washington 98105, United States
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26
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Zoogman P, Liu X, Suleiman RM, Pennington WF, Flittner DE, Al-Saadi JA, Hilton BB, Nicks DK, Newchurch MJ, Carr JL, Janz SJ, Andraschko MR, Arola A, Baker BD, Canova BP, Chan Miller C, Cohen RC, Davis JE, Dussault ME, Edwards DP, Fishman J, Ghulam A, González Abad G, Grutter M, Herman JR, Houck J, Jacob DJ, Joiner J, Kerridge BJ, Kim J, Krotkov NA, Lamsal L, Li C, Lindfors A, Martin RV, McElroy CT, McLinden C, Natraj V, Neil DO, Nowlan CR, O'Sullivan EJ, Palmer PI, Pierce RB, Pippin MR, Saiz-Lopez A, Spurr RJD, Szykman JJ, Torres O, Veefkind JP, Veihelmann B, Wang H, Wang J, Chance K. Tropospheric Emissions: Monitoring of Pollution (TEMPO). JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER 2017; 186:17-39. [PMID: 32817995 PMCID: PMC7430511 DOI: 10.1016/j.jqsrt.2016.05.008] [Citation(s) in RCA: 53] [Impact Index Per Article: 7.6] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/20/2023]
Abstract
TEMPO was selected in 2012 by NASA as the first Earth Venture Instrument, for launch between 2018 and 2021. It will measure atmospheric pollution for greater North America from space using ultraviolet and visible spectroscopy. TEMPO observes from Mexico City, Cuba, and the Bahamas to the Canadian oil sands, and from the Atlantic to the Pacific, hourly and at high spatial resolution (~2.1 km N/S×4.4 km E/W at 36.5°N, 100°W). TEMPO provides a tropospheric measurement suite that includes the key elements of tropospheric air pollution chemistry, as well as contributing to carbon cycle knowledge. Measurements are made hourly from geostationary (GEO) orbit, to capture the high variability present in the diurnal cycle of emissions and chemistry that are unobservable from current low-Earth orbit (LEO) satellites that measure once per day. The small product spatial footprint resolves pollution sources at sub-urban scale. Together, this temporal and spatial resolution improves emission inventories, monitors population exposure, and enables effective emission-control strategies. TEMPO takes advantage of a commercial GEO host spacecraft to provide a modest cost mission that measures the spectra required to retrieve ozone (O3), nitrogen dioxide (NO2), sulfur dioxide (SO2), formaldehyde (H2CO), glyoxal (C2H2O2), bromine monoxide (BrO), IO (iodine monoxide),water vapor, aerosols, cloud parameters, ultraviolet radiation, and foliage properties. TEMPO thus measures the major elements, directly or by proxy, in the tropospheric O3 chemistry cycle. Multi-spectral observations provide sensitivity to O3 in the lowermost troposphere, substantially reducing uncertainty in air quality predictions. TEMPO quantifies and tracks the evolution of aerosol loading. It provides these near-real-time air quality products that will be made publicly available. TEMPO will launch at a prime time to be the North American component of the global geostationary constellation of pollution monitoring together with the European Sentinel-4 (S4) and Korean Geostationary Environment Monitoring Spectrometer (GEMS) instruments.
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Affiliation(s)
- P Zoogman
- Harvard-Smithsonian Center for Astrophysics
| | - X Liu
- Harvard-Smithsonian Center for Astrophysics
| | | | | | | | | | | | | | | | | | - S J Janz
- NASA Goddard Space Flight Center
| | | | - A Arola
- Finnish Meteorological Institute
| | | | | | | | - R C Cohen
- University of California at Berkeley
| | - J E Davis
- Harvard-Smithsonian Center for Astrophysics
| | | | | | | | | | | | - M Grutter
- Universidad Nacional Autónoma de México
| | - J R Herman
- University of Maryland, Baltimore County
| | - J Houck
- Harvard-Smithsonian Center for Astrophysics
| | | | - J Joiner
- NASA Goddard Space Flight Center
| | | | | | | | - L Lamsal
- NASA Goddard Space Flight Center
- GESTAR, University Space Research Association
| | - C Li
- NASA Goddard Space Flight Center
- University of Maryland, Baltimore County
| | | | - R V Martin
- Harvard-Smithsonian Center for Astrophysics
- Dalhousie University
| | | | | | | | | | - C R Nowlan
- Harvard-Smithsonian Center for Astrophysics
| | | | | | - R B Pierce
- National Oceanic and Atmospheric Administration
| | | | - A Saiz-Lopez
- Instituto de Química Física Rocasolano, CSIC, Spain
| | | | | | - O Torres
- NASA Goddard Space Flight Center
| | | | | | - H Wang
- Harvard-Smithsonian Center for Astrophysics
| | | | - K Chance
- Harvard-Smithsonian Center for Astrophysics
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27
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Schroeder JR, Crawford JH, Fried A, Walega J, Weinheimer A, Wisthaler A, Müller M, Mikoviny T, Chen G, Shook M, Blake DR, Diskin G, Estes M, Thompson AM, Lefer BL, Long R, Mattson E. Formaldehyde column density measurements as a suitable pathway to estimate near-surface ozone tendencies from space. JOURNAL OF GEOPHYSICAL RESEARCH. ATMOSPHERES : JGR 2016; 121:13088-13112. [PMID: 32812915 PMCID: PMC7430524 DOI: 10.1002/2016jd025419] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/06/2023]
Abstract
In support of future satellite missions that aim to address the current shortcomings in measuring air quality from space, NASA's Deriving Information on Surface Conditions from Column and Vertically Resolved Observations Relevant to Air Quality (DISCOVER-AQ) field campaign was designed to enable exploration of relationships between column measurements of trace species relevant to air quality at high spatial and temporal resolution. In the DISCOVER-AQ data set, a modest correlation (r 2 = 0.45) between ozone (O3) and formaldehyde (CH2O) column densities was observed. Further analysis revealed regional variability in the O3-CH2O relationship, with Maryland having a strong relationship when data were viewed temporally and Houston having a strong relationship when data were viewed spatially. These differences in regional behavior are attributed to differences in volatile organic compound (VOC) emissions. In Maryland, biogenic VOCs were responsible for ~28% of CH2O formation within the boundary layer column, causing CH2O to, in general, increase monotonically throughout the day. In Houston, persistent anthropogenic emissions dominated the local hydrocarbon environment, and no discernable diurnal trend in CH2O was observed. Box model simulations suggested that ambient CH2O mixing ratios have a weak diurnal trend (±20% throughout the day) due to photochemical effects, and that larger diurnal trends are associated with changes in hydrocarbon precursors. Finally, mathematical relationships were developed from first principles and were able to replicate the different behaviors seen in Maryland and Houston. While studies would be necessary to validate these results and determine the regional applicability of the O3-CH2O relationship, the results presented here provide compelling insight into the ability of future satellite missions to aid in monitoring near-surface air quality.
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Affiliation(s)
- Jason R Schroeder
- NASA Langley Research Center, Hampton, Virginia, USA
- NASA Postdoctoral Program, NASA Langley Research Center, Hampton, Virginia, USA
| | | | - Alan Fried
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
| | - James Walega
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
| | | | - Armin Wisthaler
- Institute of Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
- Department of Chemistry, University of Oslo, Oslo, Norway
| | - Markus Müller
- Institute of Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria
| | - Tomas Mikoviny
- Department of Chemistry, University of Oslo, Oslo, Norway
| | - Gao Chen
- NASA Langley Research Center, Hampton, Virginia, USA
| | - Michael Shook
- NASA Langley Research Center, Hampton, Virginia, USA
| | - Donald R Blake
- Department of Chemistry, University of California, Irvine, California, USA
| | - Glenn Diskin
- NASA Langley Research Center, Hampton, Virginia, USA
| | - Mark Estes
- Texas Commission on Environmental Quality, Austin, Texas, USA
| | - Anne M Thompson
- Department of Meteorology, Penn State University, University Park, Pennsylvania, USA
- NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | - Barry L Lefer
- Department of Earth and Atmospheric Science, University of Houston, Houston, Texas, USA
- Now at NASA Headquarters, Washington, DC, USA
| | - Russell Long
- National Exposure Research Laboratory, U.S. EPA, Research Triangle Park, North Carolina, USA
| | - Eric Mattson
- Colorado Department of Public Health and Environment, Denver, Colorado, USA
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28
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Wolfe GM, Kaiser J, Hanisco TF, Keutsch FN, de Gouw JA, Gilman JB, Graus M, Hatch CD, Holloway J, Horowitz LW, Lee BH, Lerner BM, Lopez-Hilifiker F, Mao J, Marvin MR, Peischl J, Pollack IB, Roberts JM, Ryerson TB, Thornton JA, Veres PR, Warneke C. Formaldehyde production from isoprene oxidation across NO x regimes. ATMOSPHERIC CHEMISTRY AND PHYSICS 2016; 16:2597-2610. [PMID: 29619046 PMCID: PMC5879783 DOI: 10.5194/acp-16-2597-2016] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/04/2023]
Abstract
The chemical link between isoprene and formaldehyde (HCHO) is a strong, non-linear function of NOx (= NO + NO2). This relationship is a linchpin for top-down isoprene emission inventory verification from orbital HCHO column observations. It is also a benchmark for overall photochemical mechanism performance with regard to VOC oxidation. Using a comprehensive suite of airborne in situ observations over the Southeast U.S., we quantify HCHO production across the urban-rural spectrum. Analysis of isoprene and its major first-generation oxidation products allows us to define both a "prompt" yield of HCHO (molecules of HCHO produced per molecule of freshly-emitted isoprene) and the background HCHO mixing ratio (from oxidation of longer-lived hydrocarbons). Over the range of observed NOx values (roughly 0.1 - 2 ppbv), the prompt yield increases by a factor of 3 (from 0.3 to 0.9 ppbv ppbv-1), while background HCHO increases by a factor of 2 (from 1.6 to 3.3 ppbv). We apply the same method to evaluate the performance of both a global chemical transport model (AM3) and a measurement-constrained 0-D steady state box model. Both models reproduce the NOx dependence of the prompt HCHO yield, illustrating that models with updated isoprene oxidation mechanisms can adequately capture the link between HCHO and recent isoprene emissions. On the other hand, both models under-estimate background HCHO mixing ratios, suggesting missing HCHO precursors, inadequate representation of later-generation isoprene degradation and/or under-estimated hydroxyl radical concentrations. Detailed process rates from the box model simulation demonstrate a 3-fold increase in HCHO production across the range of observed NOx values, driven by a 100% increase in OH and a 40% increase in branching of organic peroxy radical reactions to produce HCHO.
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Affiliation(s)
- G. M. Wolfe
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, USA
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - J. Kaiser
- Department of Chemistry, University of Wisconsin-Madison, Madison, WI, USA
| | - T. F. Hanisco
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - F. N. Keutsch
- School of Engineering and Applied Sciences and Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA, USA
| | - J. A. de Gouw
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J. B. Gilman
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - M. Graus
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - C. D. Hatch
- Department of Chemistry, Hendrix College, Conway, AR, USA
| | - J. Holloway
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - L. W. Horowitz
- NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
| | - B. H. Lee
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - B. M. Lerner
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - F. Lopez-Hilifiker
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - J. Mao
- NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
- Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ
| | - M. R. Marvin
- Department of Chemistry, University of Maryland, College Park, MD, USA
| | - J. Peischl
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - I. B. Pollack
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J. M. Roberts
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - T. B. Ryerson
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J. A. Thornton
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - P. R. Veres
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - C. Warneke
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
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29
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Wolfe GM, Kaiser J, Hanisco TF, Keutsch FN, de Gouw JA, Gilman JB, Graus M, Hatch CD, Holloway J, Horowitz LW, Lee BH, Lerner BM, Lopez-Hilifiker F, Mao J, Marvin MR, Peischl J, Pollack IB, Roberts JM, Ryerson TB, Thornton JA, Veres PR, Warneke C. Formaldehyde production from isoprene oxidation across NO x regimes. ATMOSPHERIC CHEMISTRY AND PHYSICS 2016. [PMID: 29619046 DOI: 10.5194/acp-16-2597-] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Subscribe] [Scholar Register] [Indexed: 05/06/2023]
Abstract
The chemical link between isoprene and formaldehyde (HCHO) is a strong, non-linear function of NOx (= NO + NO2). This relationship is a linchpin for top-down isoprene emission inventory verification from orbital HCHO column observations. It is also a benchmark for overall photochemical mechanism performance with regard to VOC oxidation. Using a comprehensive suite of airborne in situ observations over the Southeast U.S., we quantify HCHO production across the urban-rural spectrum. Analysis of isoprene and its major first-generation oxidation products allows us to define both a "prompt" yield of HCHO (molecules of HCHO produced per molecule of freshly-emitted isoprene) and the background HCHO mixing ratio (from oxidation of longer-lived hydrocarbons). Over the range of observed NOx values (roughly 0.1 - 2 ppbv), the prompt yield increases by a factor of 3 (from 0.3 to 0.9 ppbv ppbv-1), while background HCHO increases by a factor of 2 (from 1.6 to 3.3 ppbv). We apply the same method to evaluate the performance of both a global chemical transport model (AM3) and a measurement-constrained 0-D steady state box model. Both models reproduce the NOx dependence of the prompt HCHO yield, illustrating that models with updated isoprene oxidation mechanisms can adequately capture the link between HCHO and recent isoprene emissions. On the other hand, both models under-estimate background HCHO mixing ratios, suggesting missing HCHO precursors, inadequate representation of later-generation isoprene degradation and/or under-estimated hydroxyl radical concentrations. Detailed process rates from the box model simulation demonstrate a 3-fold increase in HCHO production across the range of observed NOx values, driven by a 100% increase in OH and a 40% increase in branching of organic peroxy radical reactions to produce HCHO.
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Affiliation(s)
- G M Wolfe
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, USA
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - J Kaiser
- Department of Chemistry, University of Wisconsin-Madison, Madison, WI, USA
| | - T F Hanisco
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
| | - F N Keutsch
- School of Engineering and Applied Sciences and Department of Chemistry and Chemical Biology, Harvard University, Cambridge, MA, USA
| | - J A de Gouw
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J B Gilman
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - M Graus
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - C D Hatch
- Department of Chemistry, Hendrix College, Conway, AR, USA
| | - J Holloway
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - L W Horowitz
- NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
| | - B H Lee
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - B M Lerner
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - F Lopez-Hilifiker
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - J Mao
- NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
- Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ
| | - M R Marvin
- Department of Chemistry, University of Maryland, College Park, MD, USA
| | - J Peischl
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - I B Pollack
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J M Roberts
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - T B Ryerson
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - J A Thornton
- Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA
| | - P R Veres
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
| | - C Warneke
- Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
- Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, CO, USA
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30
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Zhu L, Jacob DJ, Kim PS, Fisher JA, Yu K, Travis KR, Mickley LJ, Yantosca RM, Sulprizio MP, De Smedt I, Abad GG, Chance K, Li C, Ferrare R, Fried A, Hair JW, Hanisco TF, Richter D, Scarino AJ, Walega J, Weibring P, Wolfe GM. Observing atmospheric formaldehyde (HCHO) from space: validation and intercomparison of six retrievals from four satellites (OMI, GOME2A, GOME2B, OMPS) with SEAC 4RS aircraft observations over the Southeast US. ATMOSPHERIC CHEMISTRY AND PHYSICS 2016; 16:13477-13490. [PMID: 29619044 PMCID: PMC5880299 DOI: 10.5194/acp-16-13477-2016] [Citation(s) in RCA: 17] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/22/2023]
Abstract
Formaldehyde (HCHO) column data from satellites are widely used as a proxy for emissions of volatile organic compounds (VOCs) but validation of the data has been extremely limited. Here we use highly accurate HCHO aircraft observations from the NASA SEAC4RS campaign over the Southeast US in August-September 2013 to validate and intercompare six retrievals of HCHO columns from four different satellite instruments (OMI, GOME2A, GOME2B and OMPS) and three different research groups. The GEOS-Chem chemical transport model is used as a common intercomparison platform. All retrievals feature a HCHO maximum over Arkansas and Louisiana, consistent with the aircraft observations and reflecting high emissions of biogenic isoprene. The retrievals are also interconsistent in their spatial variability over the Southeast US (r=0.4-0.8 on a 0.5°×0.5° grid) and in their day-to-day variability (r=0.5-0.8). However, all retrievals are biased low in the mean by 20-51%, which would lead to corresponding bias in estimates of isoprene emissions from the satellite data. The smallest bias is for OMI-BIRA, which has high corrected slant columns relative to the other retrievals and low scattering weights in its air mass factor (AMF) calculation. OMI-BIRA has systematic error in its assumed vertical HCHO shape profiles for the AMF calculation and correcting this would eliminate its bias relative to the SEAC4RS data. Our results support the use of satellite HCHO data as a quantitative proxy for isoprene emission after correction of the low mean bias. There is no evident pattern in the bias, suggesting that a uniform correction factor may be applied to the data until better understanding is achieved.
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Affiliation(s)
- Lei Zhu
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Daniel J. Jacob
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
- Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA
| | - Patrick S. Kim
- Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA
| | - Jenny A. Fisher
- Centre for Atmospheric Chemistry, School of Chemistry, University of Wollongong, Wollongong, NSW, Australia
- School of Earth and Environmental Sciences, University of Wollongong, Wollongong, NSW, Australia
| | - Karen Yu
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Katherine R. Travis
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Loretta J. Mickley
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Robert M. Yantosca
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | - Melissa P. Sulprizio
- John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
| | | | | | - Kelly Chance
- Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA
| | - Can Li
- Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland, USA
- NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
| | | | - Alan Fried
- Institute of Arctic and Alpine Research, Univ. of Colorado, Boulder, CO, USA
| | | | | | - Dirk Richter
- Institute of Arctic and Alpine Research, Univ. of Colorado, Boulder, CO, USA
| | - Amy Jo Scarino
- Science Systems and Applications, Inc., Hampton, VA, USA
| | - James Walega
- Institute of Arctic and Alpine Research, Univ. of Colorado, Boulder, CO, USA
| | - Petter Weibring
- Institute of Arctic and Alpine Research, Univ. of Colorado, Boulder, CO, USA
| | - Glenn M. Wolfe
- NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, Maryland, USA
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31
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St. Clair JM, Rivera-Rios JC, Crounse JD, Praske E, Kim MJ, Wolfe GM, Keutsch FN, Wennberg PO, Hanisco TF. Investigation of a potential HCHO measurement artifact from ISOPOOH. ATMOSPHERIC MEASUREMENT TECHNIQUES 2016; 9:4561-4568. [PMID: 29636831 PMCID: PMC5889939 DOI: 10.5194/amt-9-4561-2016] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/14/2023]
Abstract
Recent laboratory experiments have shown that a first generation isoprene oxidation product, ISOPOOH, can decompose to methyl vinyl ketone (MVK) and methacrolein (MACR) on instrument surfaces, leading to overestimates of MVK and MACR concentrations. Formaldehyde (HCHO) was suggested as a decomposition co-product, raising concern that in situ HCHO measurements may also be affected by an ISOPOOH interference. The HCHO measurement artifact from ISOPOOH for the NASA In Situ Airborne Formaldehyde instrument (ISAF) was investigated for the two major ISOPOOH isomers, (1,2)-ISOPOOH and (4,3)-ISOPOOH, under dry and humid conditions. The dry conversion of ISOPOOH to HCHO was 3±2% and 6±4% for (1,2)-ISOPOOH and (4,3)-ISOPOOH, respectively. Under humid (RH= 40-60%) conditions, conversion to HCHO was 6±4% for (1,2)-ISOPOOH and 10±5% for (4,3)-ISOPOOH. The measurement artifact caused by conversion of ISOPOOH to HCHO in the ISAF instrument was estimated for data obtained on the 2013 September 6 flight of the Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC4RS) campaign. Prompt ISOPOOH conversion to HCHO was the source for <4% of the observed HCHO, including in the high-isoprene boundary layer. Time-delayed conversion, where previous exposure to ISOPOOH affects measured HCHO later in flight, was conservatively estimated to be < 10% of observed HCHO and is significant only when high ISOPOOH sampling periods immediately precede periods of low HCHO.
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Affiliation(s)
- Jason M. St. Clair
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, 20771, USA
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, 21228, USA
| | - Jean C. Rivera-Rios
- Paulson School of Engineering and Applied Sciences and Department of Chemistry and Chemical Biology, Harvard University, Cambridge MA, 02138, USA
| | - John D. Crounse
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Eric Praske
- Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Michelle J. Kim
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Glenn M. Wolfe
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, 20771, USA
- Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, 21228, USA
| | - Frank N. Keutsch
- Department of Chemistry, University of Wisconsin-Madison, Madison, WI, 53706, USA
- Paulson School of Engineering and Applied Sciences and Department of Chemistry and Chemical Biology, Harvard University, Cambridge MA, 02138, USA
| | - Paul O. Wennberg
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, 91125, USA
- Division of Engineering and Applied Science, California Institute of Technology, Pasadena, CA, 91125, USA
| | - Thomas F. Hanisco
- Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, 20771, USA
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