1
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Brewer JF, Millet DB, Wells KC, Payne VH, Kulawik S, Vigouroux C, Cady-Pereira KE, Pernak R, Zhou M. Space-based observations of tropospheric ethane map emissions from fossil fuel extraction. Nat Commun 2024; 15:7829. [PMID: 39244593 PMCID: PMC11380669 DOI: 10.1038/s41467-024-52247-z] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/18/2023] [Accepted: 08/23/2024] [Indexed: 09/09/2024] Open
Abstract
Ethane is the most abundant non-methane hydrocarbon in the troposphere, where it impacts ozone and reactive nitrogen and is a key tracer used for partitioning emitted methane between anthropogenic and natural sources. However, quantification has been challenged by sparse observations. Here, we present a satellite-based measurement of tropospheric ethane and demonstrate its utility for fossil-fuel source quantification. An ethane spectral signal is detectable from space in Cross-track Infrared Sounder (CrIS) radiances, revealing ethane signatures associated with fires and fossil fuel production. We use machine-learning to convert these signals to ethane abundances and validate the results against surface observations (R2 = 0.66, mean CrIS/surface ratio: 0.65). The CrIS data show that the Permian Basin in Texas and New Mexico exhibits the largest persistent ethane enhancements on the planet, with regional emissions underestimated by seven-fold. Correcting this underestimate reveals Permian ethane emissions that represent at least 4-7% of the global fossil-fuel ethane source.
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Affiliation(s)
- Jared F Brewer
- University of Minnesota, Department of Soil, Water, and Climate, Saint Paul, MN, USA
| | - Dylan B Millet
- University of Minnesota, Department of Soil, Water, and Climate, Saint Paul, MN, USA.
| | - Kelley C Wells
- University of Minnesota, Department of Soil, Water, and Climate, Saint Paul, MN, USA
| | - Vivienne H Payne
- NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
| | | | - Corinne Vigouroux
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | | | - Rick Pernak
- Atmospheric and Environmental Research, Lexington, MA, USA
| | - Minqiang Zhou
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
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2
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Shutter JD, Millet DB, Wells KC, Payne VH, Nowlan CR, Abad GG. Interannual changes in atmospheric oxidation over forests determined from space. SCIENCE ADVANCES 2024; 10:eadn1115. [PMID: 38748807 PMCID: PMC11095458 DOI: 10.1126/sciadv.adn1115] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 11/22/2023] [Accepted: 04/10/2024] [Indexed: 05/19/2024]
Abstract
The hydroxyl radical (OH) is the central oxidant in Earth's troposphere, but its temporal variability is poorly understood. We combine 2012-2020 satellite-based isoprene and formaldehyde measurements to identify coherent OH changes over temperate and tropical forests with attribution to emission trends, biotic stressors, and climate. We identify a multiyear OH decrease over the Southeast United States and show that with increasingly hot/dry summers the regional chemistry could become even less oxidizing depending on competing temperature/drought impacts on isoprene. Furthermore, while global mean OH decreases during El Niño, we show that near-field effects over tropical rainforests can alternate between high/low OH anomalies due to opposing fire and biogenic emission impacts. Results provide insights into how atmospheric oxidation will evolve with changing emissions and climate.
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Affiliation(s)
- Joshua D. Shutter
- Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA
| | - Dylan B. Millet
- Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA
| | - Kelley C. Wells
- Department of Soil, Water, and Climate, University of Minnesota, St. Paul, MN 55108, USA
| | - Vivienne H. Payne
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91011, USA
| | - Caroline R. Nowlan
- Center for Astrophysics | Harvard & Smithsonian, Cambridge, MA 02138, USA
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3
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El-Sayed MMH, Parida SS, Shekhar P, Sullivan A, Hennigan CJ. Predicting Atmospheric Water-Soluble Organic Mass Reversibly Partitioned to Aerosol Liquid Water in the Eastern United States. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2023; 57:18151-18161. [PMID: 37952161 DOI: 10.1021/acs.est.3c01259] [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: 11/14/2023]
Abstract
Water-soluble organic matter (WSOM) formed through aqueous processes contributes substantially to total atmospheric aerosol, however, the impact of water evaporation on particle concentrations is highly uncertain. Herein, we present a novel approach to predict the amount of evaporated organic mass induced by sample drying using multivariate polynomial regression and random forest (RF) machine learning models. The impact of particle drying on fine WSOM was monitored during three consecutive summers in Baltimore, MD (2015, 2016, and 2017). The amount of evaporated organic mass was dependent on relative humidity (RH), WSOM concentrations, isoprene concentrations, and NOx/isoprene ratios. Different models corresponding to each class were fitted (trained and tested) to data from the summers of 2015 and 2016 while model validation was performed using summer 2017 data. Using the coefficient of determination (R2) and the root-mean-square error (RMSE), it was concluded that an RF model with 100 decision trees had the best performance (R2 of 0.81) and the lowest normalized mean error (NME < 1%) leading to low model uncertainties. The relative feature importance for the RF model was calculated to be 0.55, 0.2, 0.15, and 0.1 for WSOM concentrations, RH levels, isoprene concentrations, and NOx/isoprene ratios, respectively. The machine learning model was thus used to predict summertime concentrations of evaporated organics in Yorkville, Georgia, and Centerville, Alabama in 2016 and 2013, respectively. Results presented herein have implications for measurements that rely on sample drying using a machine learning approach for the analysis and interpretation of atmospheric data sets to elucidate their complex behavior.
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Affiliation(s)
- Marwa M H El-Sayed
- Department of Civil Engineering, Embry-Riddle Aeronautical University, Daytona Beach, Florida 32114, United States
| | - Siddharth S Parida
- Department of Civil Engineering, Embry-Riddle Aeronautical University, Daytona Beach, Florida 32114, United States
| | - Prashant Shekhar
- Department of Mathematics, Embry-Riddle Aeronautical University, Daytona Beach, Florida 32114, United States
| | - Amy Sullivan
- Department of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado 80523, United States
| | - Christopher J Hennigan
- Department of Chemical, Biochemical and Environmental Engineering, University of Maryland, Baltimore County, Baltimore, Maryland 21250, United States
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4
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Ringsdorf A, Edtbauer A, Vilà-Guerau de Arellano J, Pfannerstill EY, Gromov S, Kumar V, Pozzer A, Wolff S, Tsokankunku A, Soergel M, Sá MO, Araújo A, Ditas F, Poehlker C, Lelieveld J, Williams J. Inferring the diurnal variability of OH radical concentrations over the Amazon from BVOC measurements. Sci Rep 2023; 13:14900. [PMID: 37689759 PMCID: PMC10492859 DOI: 10.1038/s41598-023-41748-4] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/26/2023] [Accepted: 08/31/2023] [Indexed: 09/11/2023] Open
Abstract
The atmospheric oxidation of biogenic volatile organic compounds (BVOC) by OH radicals over tropical rainforests impacts local particle production and the lifetime of globally distributed chemically and radiatively active gases. For the pristine Amazon rainforest during the dry season, we empirically determined the diurnal OH radical variability at the forest-atmosphere interface region between 80 and 325 m from 07:00 to 15:00 LT using BVOC measurements. A dynamic time warping approach was applied showing that median averaged mixing times between 80 to 325 m decrease from 105 to 15 min over this time period. The inferred OH concentrations show evidence for an early morning OH peak (07:00-08:00 LT) and an OH maximum (14:00 LT) reaching 2.2 (0.2, 3.8) × 106 molecules cm-3 controlled by the coupling between BVOC emission fluxes, nocturnal NOx accumulation, convective turbulence, air chemistry and photolysis rates. The results were evaluated with a turbulence resolving transport (DALES), a regional scale (WRF-Chem) and a global (EMAC) atmospheric chemistry model.
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Affiliation(s)
- A Ringsdorf
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany.
| | - A Edtbauer
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - J Vilà-Guerau de Arellano
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
- Meteorology and Air Quality Section, Wageningen University, Wageningen, The Netherlands
| | - E Y Pfannerstill
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - S Gromov
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - V Kumar
- Satellite Remote Sensing Group, Max Planck Institute for Chemistry, Mainz, Germany
| | - A Pozzer
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - S Wolff
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - A Tsokankunku
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - M Soergel
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
- Friedrich-Alexander-Universität Erlangen-Nürnberg, Sachgebiet Arbeitssicherheit, Erlangen, Germany
| | - M O Sá
- Instituto Nacional de Pesquisas da Amazônia (INPA), Manaus, CEP 69067-375, Brazil
| | - A Araújo
- Empresa Brasileira de Pesquisa Agropecuária (Embrapa) Amazonia Oriental, Belém, CEP 66095-100, Brazil
| | - F Ditas
- Department of Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
- Hessian Agency for Nature Conservation, Environment and Geology, Wiesbaden, Germany
| | - C Poehlker
- Department of Multiphase Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
| | - J Lelieveld
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
- Climate and Atmosphere Research Center, The Cyprus Institute, 1645, Nicosia, Cyprus
| | - J Williams
- Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany.
- Climate and Atmosphere Research Center, The Cyprus Institute, 1645, Nicosia, Cyprus.
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5
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Stewart JT, Hino L, Pavlonnis C, Reyna KR, Vo BLN. Rotationally Resolved Infrared Spectroscopy of Supersonic Jet-Cooled Isoprene. J Phys Chem A 2023. [PMID: 37235782 DOI: 10.1021/acs.jpca.3c02272] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 05/28/2023]
Abstract
The high-resolution infrared spectrum of isoprene has been observed under supersonic jet-cooled conditions in the region of the ν26 vibrational band near 992 cm-1. The spectrum was assigned and fit using a standard asymmetric top Hamiltonian, and an acceptable fit was obtained for transitions to excited state energy levels with J ≤ 6, with an error in the fit of 0.002 cm-1. For excited state energy levels with J > 6, a perturbation was present that prevented fitting using the standard asymmetric top Hamiltonian. Based on previous anharmonic frequency calculations and observed vibrational bands of isoprene, the perturbation is most likely caused by Coriolis coupling between the ν26 and ν17 vibrations or a combination band that lies near the ν26 band. The excited state rotational constants from the fit show reasonable agreement with previous anharmonic calculations performed at the MP2/cc-pVTZ level of theory. The jet-cooled spectrum is compared with previous high-resolution measurements of this band at room temperature and shows that understanding the perturbation will be necessary to accurately model this vibrational band.
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Affiliation(s)
- Jacob T Stewart
- Department of Chemistry, Connecticut College, New London, Connecticut 06320, United States
| | - Lauren Hino
- Department of Chemistry, Connecticut College, New London, Connecticut 06320, United States
| | - Carter Pavlonnis
- Department of Chemistry, Connecticut College, New London, Connecticut 06320, United States
| | - Katarina R Reyna
- Department of Chemistry, Connecticut College, New London, Connecticut 06320, United States
| | - Binh L N Vo
- Department of Chemistry, Connecticut College, New London, Connecticut 06320, United States
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6
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Lou C, Jiang F, Tian X, Zou Q, Zheng Y, Shen Y, Feng S, Chen J, Zhang L, Jia M, Xu J. Modeling the biogenic isoprene emission and its impact on ozone pollution in Zhejiang province, China. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 865:161212. [PMID: 36586687 DOI: 10.1016/j.scitotenv.2022.161212] [Citation(s) in RCA: 2] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/14/2022] [Revised: 12/22/2022] [Accepted: 12/23/2022] [Indexed: 06/17/2023]
Abstract
Isoprene is the most abundantly emitted biogenic volatile organic compound (BVOC), which plays an essential role in producing tropospheric ozone (O3). However, the simulations of isoprene emissions have not been sufficiently verified over Yangtze River Delta (YRD), and few studies have specifically addressed its impact on O3 formation. In this study, we simulated the isoprene emissions in Zhejiang Province (ZJ), a region with the largest BVOC emission in YRD, in August 2020 using the Model of Emissions of Gases and Aerosols from Nature (MEGAN) and the latest Moderate Resolution Imaging Spectroradiometer (MODIS) products, and investigated its contributions to O3 using the Weather Research and Forecasting (WRF)-Community Multiscale Air Quality (CMAQ) model. The model has a good performance on isoprene simulations over urban and suburban areas, with mean biases of -0.16-0.12 ppb, but underestimated the concentrations at forest sites (mainly due to bamboo). Regionally, the simulated formaldehyde concentrations over forests agree well with the satellite observations. In August 2020, the total isoprene emission in ZJ was 125.1 GgC, with higher emissions in western ZJ and relatively lower emissions in eastern coastal regions. The spatial pattern of isoprene concentrations is similar to its emissions, and the maximum daytime average concentrations are above 3.5 ppb. The spatial pattern of its contribution to daily maximum 8 h average O3 concentrations is significantly different from the emissions and concentrations, which shows a higher impact in northern ZJ (>6 ppb) and relatively lower impact in southern ZJ (1-3 ppb). The mean contribution over ZJ is 8.9 %, with daily variation in the range of 3.1 % to 13.4 %. For different cities, the monthly mean contribution is in the range of 4.6 % to 14.3 %, and the maximum daily contribution reaches about 25 %. These findings help understand the summertime O3 pollution in ZJ and the YRD region of China.
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Affiliation(s)
- Chenxi Lou
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Fei Jiang
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China; Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China; Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing 210023, China.
| | - Xudong Tian
- Zhejiang Ecological and Environmental Monitoring Center, Hangzhou 310012, China; Zhejiang Key Laboratory of Ecological and Environmental Monitoring, Forewarning and Quality Control, Hangzhou 310012, China
| | - Qiaoli Zou
- Zhejiang Ecological and Environmental Monitoring Center, Hangzhou 310012, China; Zhejiang Key Laboratory of Ecological and Environmental Monitoring, Forewarning and Quality Control, Hangzhou 310012, China
| | - Yanhua Zheng
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Yang Shen
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Shuzhuang Feng
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Jiansong Chen
- Zhejiang Hangzhou Ecological and Environment Monitoring Center, Hangzhou 310007, China
| | - Lingyu Zhang
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Mengwei Jia
- Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, International Institute for Earth System Science, Nanjing University, Nanjing 210023, China
| | - Jiawei Xu
- School of Atmospheric Sciences, Nanjing University, Nanjing 210023, China
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7
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Zhang Z, Wang C, Zhao Y, Zhao Y, Li G, Xie H, Jiang L. Autoxidation Mechanism and Kinetics of Methacrolein in the Atmosphere. J Phys Chem A 2023; 127:2819-2829. [PMID: 36939326 DOI: 10.1021/acs.jpca.3c00128] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 03/21/2023]
Abstract
Elucidating the autoxidation of volatile organic compounds (VOCs) is crucial to understanding the formation mechanism of secondary organic aerosols, but it has been proven to be challenging due to the complexity of reactions under atmospheric conditions. Here, we report a comprehensive theoretical study of atmospheric autoxidation in VOCs exemplified by the atmospherically important methacrolein (MACR), a major oxidation product of isoprene. The results indicate that the Cl-adducts and H-abstraction products of MACR readily react with O2 and undergo subsequent isomerizations via H-shift and cyclization, forming a large variety of lowly and highly oxygenated organic molecules. In particular, the first- and third-generation oxidation products derived from the Cl-adducts and the methyl-H-abstraction complexes are dominated in the atmospheric autoxidation, for which the fractional yields are remarkably affected by the NO concentration. The present findings have important implications for a systematical understanding of the oxidation processes of isoprene-derived compounds in the atmospheric environments.
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Affiliation(s)
- Zhaoyan Zhang
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China.,University of Chinese Academy of Sciences, 19A Yuquan Road, Beijing 100049, China
| | - Chong Wang
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China.,University of Chinese Academy of Sciences, 19A Yuquan Road, Beijing 100049, China
| | - Yingqi Zhao
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China.,University of Chinese Academy of Sciences, 19A Yuquan Road, Beijing 100049, China
| | - Ya Zhao
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China
| | - Gang Li
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China
| | - Hua Xie
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China
| | - Ling Jiang
- State Key Laboratory of Molecular Reaction Dynamics, Dalian Institute of Chemical Physics, Chinese Academy of Sciences, 457 Zhongshan Road, Dalian 116023, China.,Hefei National Laboratory, Hefei 230088, China
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8
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Wasti S, Wang Y. Spatial and temporal analysis of HCHO response to drought in South Korea. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 852:158451. [PMID: 36063934 DOI: 10.1016/j.scitotenv.2022.158451] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/24/2022] [Revised: 08/29/2022] [Accepted: 08/29/2022] [Indexed: 06/15/2023]
Abstract
Though drought is known to affect biogenic emissions of volatile organic compounds (BVOC), its effect on isoprene and formaldehyde (HCHO), a high yield product of isoprene, has not been investigated in East Asia where incidences of drought have increased in recent years. In this work, we analyzed the impact of drought on HCHO in the South Korea region during the summer period (June, July, and August) from 2005 to 2018 and found increased HCHO due to drought. The tropospheric HCHO column density retrieved by OMI increased by 8.02 % during extreme drought compared to the non-drought period, whereas no significant effect of drought on the NO2 column was found. Regional variation of HCHO response to drought correlates significantly with the tree percentage of the region. This correlation indicates that the drought-led HCHO increases are most likely driven by the increase in isoprene emissions during drought. Indeed, model predicts isoprene emissions to be higher by 27.87 % during the extreme drought compared to the non-drought period in South Korea. From 2005 to 2018, the HCHO column has been increasing in South Korea by 0.16 × 1015 molecules/cm2/year (1.56 % per year) during summer months, correlated with the increasing incidences of drought. HCHO increase is linked to higher ozone as most of South Korea is in the NOx-saturated or transitional regime.
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Affiliation(s)
- Shailaja Wasti
- Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, USA
| | - Yuxuan Wang
- Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX, USA.
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9
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Wang H, Lu X, Seco R, Stavrakou T, Karl T, Jiang X, Gu L, Guenther AB. Modeling Isoprene Emission Response to Drought and Heatwaves Within MEGAN Using Evapotranspiration Data and by Coupling With the Community Land Model. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS 2022; 14:e2022MS003174. [PMID: 37035629 PMCID: PMC10078486 DOI: 10.1029/2022ms003174] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 05/02/2022] [Revised: 10/18/2022] [Accepted: 11/08/2022] [Indexed: 06/19/2023]
Abstract
We introduce two new drought stress algorithms designed to simulate isoprene emission with the Model of Emissions of Gases and Aerosols from Nature (MEGAN) model. The two approaches include the representation of the impact of drought on isoprene emission with a simple empirical approach for offline MEGAN applications and a more process-based approach for online MEGAN in Community Land Model (CLM) simulations. The two versions differ in their implementation of leaf-temperature impacts of mild drought. For the online version of MEGAN that is coupled to CLM, the impact of drought on leaf temperature is simulated directly and the calculated leaf temperature is considered for the estimation of isoprene emission. For the offline version, we apply an empirical algorithm derived from whole-canopy flux measurements for simulating the impact of drought ranging from mild to severe stage. In addition, the offline approach adopts the ratio (f PET) of actual evapotranspiration to potential evapotranspiration to quantify the severity of drought instead of using soil moisture. We applied the two algorithms in the CLM-CAM-chem (the Community Atmosphere Model with Chemistry) model to simulate the impact of drought on isoprene emission and found that drought can decrease isoprene emission globally by 11% in 2012. We further compared the formaldehyde (HCHO) vertical column density simulated by CAM-chem to satellite HCHO observations. We found that the proposed drought algorithm can improve the match with the HCHO observations during droughts, but the performance of the drought algorithm is limited by the capacity of the model to capture the severity of drought.
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Affiliation(s)
- Hui Wang
- Department of Earth System ScienceUniversity of California IrvineIrvineCAUSA
| | - Xinchen Lu
- Department of Environmental Science, Policy and ManagementUniversity of California BerkeleyBerkeleyCAUSA
| | - Roger Seco
- Institute of Environmental Assessment and Water Research (IDAEA‐CSIC)BarcelonaSpain
| | | | - Thomas Karl
- Department of Atmospheric and Cryospheric SciencesUniversity of InnsbruckInnsbruckAustria
| | - Xiaoyan Jiang
- Department of Earth System ScienceUniversity of California IrvineIrvineCAUSA
| | - Lianhong Gu
- Environmental Sciences DivisionOak Ridge National LaboratoryClimate Change Science InstituteOak RidgeTNUSA
| | - Alex B. Guenther
- Department of Earth System ScienceUniversity of California IrvineIrvineCAUSA
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10
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Palmer PI, Woodwark AJP, Finch DP, Taylor TE, Butz A, Tamminen J, Bösch H, Eldering A, Vincent-Bonnieu S. 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] [Grants] [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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Affiliation(s)
- Paul I Palmer
- School of GeoSciences, University of Edinburgh, Edinburgh, UK.
- National Centre for Earth Observation, University of Edinburgh, Edinburgh, UK.
| | | | - Douglas P Finch
- School of GeoSciences, University of Edinburgh, Edinburgh, UK
| | - Thomas E Taylor
- Cooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, CO, USA
| | - André Butz
- Institute of Environmental Physics, Heidelberg University, Heidelberg, Germany
| | | | - Hartmut Bösch
- National Centre for Earth Observation, University of Leicester, Leicester, UK
- Earth Observation Science, School of Physics and Astronomy, University of Leicester, Leicester, UK
| | - Annmarie Eldering
- Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA
| | - Sebastien Vincent-Bonnieu
- Directorate of Human and Robotic Exploration Programmes, European Space Agency - ESTEC, Noordwijk-ZH, The Netherlands
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11
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Han Z, Zhang Y, Zhang H, Ge X, Gu D, Liu X, Bai J, Ma Z, Tan Y, Zhu F, Xia S, Du J, Tan Y, Shu X, Tang J, Sun Y. Impacts of Drought and Rehydration Cycles on Isoprene Emissions in Populus nigra Seedlings. INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH 2022; 19:14528. [PMID: 36361409 PMCID: PMC9655116 DOI: 10.3390/ijerph192114528] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 09/23/2022] [Revised: 10/28/2022] [Accepted: 11/03/2022] [Indexed: 06/16/2023]
Abstract
The volatile organic compounds emitted by plants significantly impact the atmospheric environment. The impacts of drought stress on the biogenic volatile organic compound (BVOC) emissions of plants are still under debate. In this study, the effects of two drought-rehydration cycle groups with different durations on isoprene emissions from Populus nigra (black poplar) seedlings were studied. The P. nigra seedlings were placed in a chamber that controlled the soil water content, radiation, and temperature. The daily emissions of isoprene and physiological parameters were measured. The emission rates of isoprene (Fiso) reached the maximum on the third day (D3), increasing by 58.0% and 64.2% compared with the controlled groups, respectively, and then Fiso significantly decreased. Photosynthesis decreased by 34.2% and 21.6% in D3 in the first and second groups, respectively. After rehydration, Fiso and photosynthesis recovered fully in two groups. However, Fiso showed distinct inconsistencies in two groups, and the recovery rates of Fiso in the second drought group were slower than the recovery rates of Fiso in the first groups. The response of BVOC emissions during the drought-rehydration cycle was classified into three phases, including stimulated, inhibited, and restored after rehydration. The emission pattern of isoprene indicated that isoprene played an important role in the response of plants to drought stress. A drought-rehydration model was constructed, which indicated the regularity of BVOC emissions in the drought-rehydration cycle. BVOC emissions were extremely sensitive to drought, especially during droughts of short duration. Parameters in computational models related to BVOC emissions of plants under drought stress should be continuously improved.
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Affiliation(s)
- Zhiyu Han
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Yisheng Zhang
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
- Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou 511486, China
| | - Houyong Zhang
- Jinan Ecology and Environment Monitoring Center of Shandong Province, Jinan 250101, China
| | - Xuan Ge
- Jinan Ecology and Environment Monitoring Center of Shandong Province, Jinan 250101, China
| | - Dasa Gu
- Division of Environment and Sustainability, The Hong Kong University of Science and Technology, Hong Kong 999077, China
| | - Xiaohuan Liu
- Key Lab of Marine Environment and Ecology, Ministry of Education, Ocean University of China, Qingdao 266100, China
| | - Jianhui Bai
- LAGEO, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
| | - Zizhen Ma
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Yan Tan
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Feng Zhu
- Hebei Key Laboratory of Soil Ecology, Key Laboratory of Agricultural Water Resources, Center for Agricultural Resources Research, Institute of Genetic and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang 050022, China
| | - Shiyong Xia
- School of Environment and Energy, Peking University, Shenzhen 518055, China
| | - Jinhua Du
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Yuran Tan
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Xiao Shu
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Jingchao Tang
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
| | - Yingjie Sun
- School of Environmental and Municipal Engineering, Qingdao University of Technology, Qingdao 266520, China
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12
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Selimovic V, Ketcherside D, Chaliyakunnel S, Wielgasz C, Permar W, Angot H, Millet DB, Fried A, Helmig D, Hu L. Atmospheric biogenic volatile organic compounds in the Alaskan Arctic tundra: constraints from measurements at Toolik Field Station. ATMOSPHERIC CHEMISTRY AND PHYSICS 2022; 22:14037-14058. [PMID: 37476609 PMCID: PMC10358744 DOI: 10.5194/acp-22-14037-2022] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Indexed: 07/22/2023]
Abstract
The Arctic is a climatically sensitive region that has experienced warming at almost 3 times the global average rate in recent decades, leading to an increase in Arctic greenness and a greater abundance of plants that emit biogenic volatile organic compounds (BVOCs). These changes in atmospheric emissions are expected to significantly modify the overall oxidative chemistry of the region and lead to changes in VOC composition and abundance, with implications for atmospheric processes. Nonetheless, observations needed to constrain our current understanding of these issues in this critical environment are sparse. This work presents novel atmospheric in situ proton-transfer-reaction time-of-flight mass spectrometry (PTR-ToF-MS) measurements of VOCs at Toolik Field Station (TFS; 68°38' N, 149°36' W), in the Alaskan Arctic tundra during May-June 2019. We employ a custom nested grid version of the GEOS-Chem chemical transport model (CTM), driven with MEGANv2.1 (Model of Emissions of Gases and Aerosols from Nature version 2.1) biogenic emissions for Alaska at 0.25° × 0.3125° resolution, to interpret the observations in terms of their constraints on BVOC emissions, total reactive organic carbon (ROC) composition, and calculated OH reactivity (OHr) in this environment. We find total ambient mole fraction of 78 identified VOCs to be 6.3 ± 0.4 ppbv (10.8 ± 0.5 ppbC), with overwhelming (> 80 %) contributions are from short-chain oxygenated VOCs (OVOCs) including methanol, acetone and formaldehyde. Isoprene was the most abundant terpene identified. GEOS-Chem captures the observed isoprene (and its oxidation products), acetone and acetaldehyde abundances within the combined model and observation uncertainties (±25 %), but underestimates other OVOCs including methanol, formaldehyde, formic acid and acetic acid by a factor of 3 to 12. The negative model bias for methanol is attributed to underestimated biogenic methanol emissions for the Alaskan tundra in MEGANv2.1. Observed formaldehyde mole fractions increase exponentially with air temperature, likely reflecting its biogenic precursors and pointing to a systematic model underprediction of its secondary production. The median campaign-calculated OHr from VOCs measured at TFS was 0.7 s-1, roughly 5 % of the values typically reported in lower-latitude forested ecosystems. Ten species account for over 80 % of the calculated VOC OHr, with formaldehyde, isoprene and acetaldehyde together accounting for nearly half of the total. Simulated OHr based on median-modeled VOCs included in GEOS-Chem averages 0.5 s-1 and is dominated by isoprene (30 %) and monoterpenes (17 %). The data presented here serve as a critical evaluation of our knowledge of BVOCs and ROC budgets in high-latitude environments and represent a foundation for investigating and interpreting future warming-driven changes in VOC emissions in the Alaskan Arctic tundra.
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Affiliation(s)
- Vanessa Selimovic
- Department of Chemistry and Biochemistry, University of Montana, Missoula, MT, USA
| | - Damien Ketcherside
- Department of Chemistry and Biochemistry, University of Montana, Missoula, MT, USA
| | | | - Catherine Wielgasz
- Department of Chemistry and Biochemistry, University of Montana, Missoula, MT, USA
| | - Wade Permar
- Department of Chemistry and Biochemistry, University of Montana, Missoula, MT, USA
| | - Hélène Angot
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, USA
| | - Dylan B. Millet
- Department of Soil, Water, and Climate, University of Minnesota Twin Cities, St Paul, MN, USA
| | - Alan Fried
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, USA
| | | | - Lu Hu
- Department of Chemistry and Biochemistry, University of Montana, Missoula, MT, USA
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13
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Mears KL, Kutzleb MA, Stennett CR, Fettinger JC, Kaseman DC, Yu P, Vasko P, Power PP. Terpene dispersion energy donor ligands in borane complexes. Chem Commun (Camb) 2022; 58:9910-9913. [PMID: 35979664 DOI: 10.1039/d2cc04203g] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
Structural characterization of the complex [B(β-pinane)3] (1) reveals non-covalent H⋯H contacts that are consistent with the generation of London dispersion energies involving the β-pinane ligand frameworks. The homolytic fragmentations of 1, and camphane and sabinane analogues ([B(camphane)3] (2) and [B(sabinane)3] (3)) were studied computationally. Isodesmic exchange results showed that London dispersion interactions are highly dependent on the terpene's stereochemistry, with the β-pinane framework providing the greatest dispersion free energy (ΔG = -7.9 kcal mol-1) with Grimme's dispersion correction (D3BJ) employed. PMe3 was used to coordinate to [B(β-pinane)3], giving the complex [Me3P-B(β-pinane)3] (4), which displayed a dynamic coordination equilibrium in solution. The association process was found to be slightly endergonic at 302 K (ΔG = +0.29 kcal mol-1).
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Affiliation(s)
- Kristian L Mears
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - Michelle A Kutzleb
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - Cary R Stennett
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - James C Fettinger
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - Derrick C Kaseman
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - Ping Yu
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
| | - Petra Vasko
- Department of Chemistry, University of Helsinki, PO Box 55 (A. I. Virtasen aukio 1), 00014, Finland.
| | - Philip P Power
- Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, USA.
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14
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Zhu Q, Laughner JL, Cohen RC. Combining Machine Learning and Satellite Observations to Predict Spatial and Temporal Variation of near Surface OH in North American Cities. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:7362-7371. [PMID: 35302754 DOI: 10.1021/acs.est.1c05636] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/14/2023]
Abstract
The hydroxyl radical (OH) is the primary cleansing agent in the atmosphere. The abundance of OH in cities initiates the removal of local pollutants; therefore, it serves as the key species describing the urban chemical environment. We propose a machine learning (ML) approach as an efficient alternative to OH simulation using a computationally expensive chemical transport model. The ML model is trained on the parameters simulated from the WRF-Chem model, and it suggests that six predictive parameters are capable of explaining 76% of the OH variability. The parameters are the tropospheric NO2 column, the tropospheric HCHO column, J(O1D), H2O, temperature, and pressure. We then use observations of the tropospheric NO2 column and HCHO column from OMI as input to the ML model to enable measurement-based prediction of daily near surface OH at 1:30 pm local time across 49 North American cities over the course of 10 years between 2005 and 2014. The result is validated by comparing the OH predictions to measurements of isoprene, which has a source that is uncorrelated with OH and is removed rapidly and almost exclusively by OH in the daytime. We demonstrate that the predicted OH is, as expected, anticorrelated with isoprene. We also show that this ML model is consistent with our understanding of OH chemistry given the solely data-driven nature.
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Affiliation(s)
- Qindan Zhu
- Department of Earth and Planetary Science, University of California at Berkeley, Berkeley, California 94720, United States
| | - Joshua L Laughner
- Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, United States
| | - Ronald C Cohen
- Department of Earth and Planetary Science, University of California at Berkeley, Berkeley, California 94720, United States
- Department of Chemistry, University of California at Berkeley, Berkeley, California 94720, United States
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15
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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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16
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Wang L, Li B, Dionysiou DD, Chen B, Yang J, Li J. Overlooked Formation of H 2O 2 during the Hydroxyl Radical-Scavenging Process When Using Alcohols as Scavengers. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2022; 56:3386-3396. [PMID: 35230098 DOI: 10.1021/acs.est.1c03796] [Citation(s) in RCA: 42] [Impact Index Per Article: 21.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/14/2023]
Abstract
Hydroxyl radical (•OH) is an active species widely reported in studies across many scientific fields, and hence, its reliable analysis is vitally important. Currently, alcohols are commonly used as scavengers for •OH determination. However, the impacts of alcohols on the reliability of •OH detection remain unknown. In this study, we found that adding different types and different amounts of alcohols in water samples treated with ultraviolet irradiation undesirably produced substantial amounts of hydrogen peroxide (H2O2), which is a known •OH precursor. This means that the conventional •OH determination method using alcohols is likely unreliable or even misleading. Through careful investigation, we revealed an overlooked reaction pathway during H2O2 and •OH transformations. Varying oxygen concentrations, pHs, alcohol dosages, and types altered H2O2 formation, which can affect •OH determination accuracy. Among alcohols, n-butanol is the best scavenger because it quenches •OH rapidly but re-forms little H2O2.
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Affiliation(s)
- Lei Wang
- State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Shenzhen 518055, China
- Aquatic Plant Research Center, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China
| | - Boqiang Li
- State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Shenzhen 518055, China
| | - Dionysios D Dionysiou
- Department of Chemical and Environmental Engineering, University of Cincinnati, Cincinnati, Ohio 45221-0012, United States
| | - Baiyang Chen
- State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Shenzhen 518055, China
| | - Jie Yang
- State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Shenzhen 518055, China
| | - Juan Li
- State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology, Shenzhen 518055, China
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17
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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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18
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Palmer PI, Marvin MR, Siddans R, Kerridge BJ, Moore DP. Nocturnal survival of isoprene linked to formation of upper tropospheric organic aerosol. Science 2022; 375:562-566. [PMID: 35113698 DOI: 10.1126/science.abg4506] [Citation(s) in RCA: 8] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/26/2022]
Abstract
Isoprene is emitted mainly by terrestrial vegetation and is the dominant volatile organic compound (VOC) in Earth's atmosphere. It plays key roles in determining the oxidizing capacity of the troposphere and the formation of organic aerosol. Daytime infrared satellite observations of isoprene reported here broadly agree with emission inventories, but we found substantial differences in the locations and magnitudes of isoprene hotspots, consistent with a recent study. The corresponding nighttime infrared observations reveal unexpected hotspots over tropical South America, the Congo basin, and Southeast Asia. We used an atmospheric chemistry model to link these nighttime isoprene measurements to low-NOx regions with high biogenic VOC emissions; at sunrise the remaining isoprene can lead to the production of epoxydiols and subsequently to the widespread seasonal production of organic aerosol in the tropical upper troposphere.
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Affiliation(s)
- Paul I Palmer
- National Centre for Earth Observation, University of Edinburgh, Edinburgh, UK.,School of GeoSciences, University of Edinburgh, Edinburgh, UK
| | - Margaret R Marvin
- National Centre for Earth Observation, University of Edinburgh, Edinburgh, UK.,School of GeoSciences, University of Edinburgh, Edinburgh, UK
| | - Richard Siddans
- National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK.,Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
| | - Brian J Kerridge
- National Centre for Earth Observation, STFC Rutherford Appleton Laboratory, Chilton, UK.,Remote Sensing Group, STFC Rutherford Appleton Laboratory, Chilton, UK
| | - David P Moore
- National Centre for Earth Observation, University of Leicester, Leicester, UK.,School of Physics and Astronomy, University of Leicester, Leicester, UK
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19
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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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