1
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Ma C, Su H, Lelieveld J, Randel W, Yu P, Andreae MO, Cheng Y. Smoke-charged vortex doubles hemispheric aerosol in the middle stratosphere and buffers ozone depletion. SCIENCE ADVANCES 2024; 10:eadn3657. [PMID: 38996024 PMCID: PMC11244531 DOI: 10.1126/sciadv.adn3657] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/06/2023] [Accepted: 06/10/2024] [Indexed: 07/14/2024]
Abstract
Australian mega-wildfires in the summer of 2019-2020 injected smoke into the stratosphere, causing strong ozone depletion in the lower stratosphere. Here, we model the smoke plume and reproduce its unexpected trajectory toward the middle stratosphere at ~35-kilometer altitude. We show that a smoke-charged vortex (SCV) induced and maintained by absorbing aerosols played a key role in lofting pollutants from the lower stratosphere and nearly doubled the southern hemispheric aerosol burden in the middle stratosphere. The SCV caused a redistribution of stratospheric aerosols, which boosted heterogeneous chemistry in the middle stratosphere and enhanced ozone production, compensating for up to 70% of the ozone depletion in the lower stratosphere. As global warming continues, we expect a growing frequency and importance of SCVs in promoting the impacts of wildfires on stratospheric aerosols and chemistry.
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Affiliation(s)
- Chaoqun Ma
- Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - Hang Su
- Key Laboratory of Atmospheric Environment and Extreme Meteorology, Institute for Atmospheric Physics, Chinese Academy of Science, Beijing 100029, China
| | - Jos Lelieveld
- Atmospheric Chemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
| | - William Randel
- Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder, CO 80307, USA
| | - Pengfei Yu
- Institute for Environmental and Climate Research, Jinan University, Guangzhou 510630, China
| | - Meinrat O. Andreae
- Biogeochemistry Department, Max Planck Institute for Chemistry, 55128 Mainz, Germany
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92037, USA
| | - Yafang Cheng
- Minerva Research Group, Max Planck Institute for Chemistry, 55128 Mainz, Germany
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2
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Gill RL, Fleck R, Chau K, Westerhausen MT, Lockwood TE, Violi JP, Irga PJ, Doblin MA, Torpy FR. Fine particle pollution during megafires contains potentially toxic elements. ENVIRONMENTAL POLLUTION (BARKING, ESSEX : 1987) 2024; 344:123306. [PMID: 38185362 DOI: 10.1016/j.envpol.2024.123306] [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: 08/29/2023] [Revised: 01/04/2024] [Accepted: 01/04/2024] [Indexed: 01/09/2024]
Abstract
Wildfires that raged across Australia during the 2019-2020 'Black Summer' produced an enormous quantity of particulate matter (PM) pollution, with plumes that cloaked many urban centres and ecosystems along the eastern seaboard. This has motivated a need to understand the magnitude and nature of PM exposure, so that its impact on both built and natural environments can be more accurately assessed. Here we present the potentially toxic fingerprint of PM captured by building heating, ventilation, and air conditioning filters in Sydney, Australia during the peak of the Wildfires, and from ambient urban emissions one year later (Reference period). Atmospheric PM and meteorological monitoring data were also assessed to determine the magnitude and source of high PM exposure. The wildfires were a major source of PM pollution in Sydney, exceeding the national standards on 19 % of days between November-February. Wildfire particles were finer and more spherical compared to Reference PM, with count median diameters of 892.1 ± 23.1 versus 1484.8 ± 96.7 nm (mean ± standard error). On an equal-mass basis, differences in potentially toxic elements were predominantly due to higher SO42--S (median 20.4 vs 4.7 mg g-1) and NO3--N (2.4 vs 1.2 mg g-1) in Wildfire PM, and higher PO43--P (10.4 vs 1.4 mg g-1) in Reference PM. Concentrations of remaining elements were similar or lower than Reference PM, except for enrichments to F-, Cl-, dissolved Mn, and particulate Mn, Co and Sb. Fractional solubilities of trace elements were similar or lower than Reference PM, except for enhanced Hg (12.1 vs 1.0 %) and greater variability in Cd, Hg and Mn solubility, which displayed upper quartiles exceeding that of Reference PM. These findings contribute to our understanding of human and ecosystem exposures to the toxic components of mixed smoke plumes, especially in regions downwind of the source.
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Affiliation(s)
- Raissa L Gill
- Productive Coasts, Climate Change Cluster, University of Technology Sydney, Ultimo, NSW, 2007, Australia; Plants and Environmental Quality Research Group, School of Life Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia.
| | - Robert Fleck
- Plants and Environmental Quality Research Group, School of Life Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia
| | - Ky Chau
- Plants and Environmental Quality Research Group, School of Life Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia
| | - Mika T Westerhausen
- Hyphenated Mass Spectrometry Laboratory, School of Mathematical and Physical Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia
| | - Thomas E Lockwood
- Hyphenated Mass Spectrometry Laboratory, School of Mathematical and Physical Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia
| | - Jake P Violi
- School of Chemistry, University of New South Wales, Sydney, NSW, 2052, Australia
| | - Peter J Irga
- Plants and Environmental Quality Research Group, School of Civil and Environmental Engineering, University of Technology Sydney, Ultimo, NSW, 2007, Australia
| | - Martina A Doblin
- Productive Coasts, Climate Change Cluster, University of Technology Sydney, Ultimo, NSW, 2007, Australia; Sydney Institute of Marine Science, Mosman, NSW, 2088, Australia
| | - Fraser R Torpy
- Plants and Environmental Quality Research Group, School of Life Sciences, University of Technology Sydney, Ultimo, NSW, 2007, Australia
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3
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Tastassa AC, Sharaby Y, Lang-Yona N. Aeromicrobiology: A global review of the cycling and relationships of bioaerosols with the atmosphere. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 912:168478. [PMID: 37967625 DOI: 10.1016/j.scitotenv.2023.168478] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/10/2023] [Revised: 10/31/2023] [Accepted: 11/08/2023] [Indexed: 11/17/2023]
Abstract
Airborne microorganisms and biological matter (bioaerosols) play a key role in global biogeochemical cycling, human and crop health trends, and climate patterns. Their presence in the atmosphere is controlled by three main stages: emission, transport, and deposition. Aerial survival rates of bioaerosols are increased through adaptations such as ultra-violet radiation and desiccation resistance or association with particulate matter. Current research into modern concerns such as climate change, global gene transfer, and pathogenicity often neglects to consider atmospheric involvement. This comprehensive review outlines the transpiring of bioaerosols across taxa in the atmosphere, with significant focus on their interactions with environmental elements including abiotic factors (e.g., atmospheric composition, water cycle, and pollution) and events (e.g., dust storms, hurricanes, and wildfires). The aim of this review is to increase understanding and shed light on needed research regarding the interplay between global atmospheric phenomena and the aeromicrobiome. The abundantly documented bacteria and fungi are discussed in context of their cycling and human health impacts. Gaps in knowledge regarding airborne viral community, the challenges and importance of studying their composition, concentrations and survival in the air are addressed, along with understudied plant pathogenic oomycetes, and archaea cycling. Key methodologies in sampling, collection, and processing are described to provide an up-to-date picture of ameliorations in the field. We propose optimization to microbiological methods, commonly used in soil and water analysis, that adjust them to the context of aerobiology, along with other directions towards novel and necessary advancements. This review offers new perspectives into aeromicrobiology and calls for advancements in global-scale bioremediation, insights into ecology, climate change impacts, and pathogenicity transmittance.
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Affiliation(s)
- Ariel C Tastassa
- Civil and Environmental Engineering, Technion - Israel Institute of Technology, 3200003 Haifa, Israel
| | - Yehonatan Sharaby
- Civil and Environmental Engineering, Technion - Israel Institute of Technology, 3200003 Haifa, Israel
| | - Naama Lang-Yona
- Civil and Environmental Engineering, Technion - Israel Institute of Technology, 3200003 Haifa, Israel.
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4
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Xue C, Krysztofiak G, Ren Y, Cai M, Mercier P, Fur FL, Robin C, Grosselin B, Daële V, McGillen MR, Mu Y, Catoire V, Mellouki A. A study on wildfire impacts on greenhouse gas emissions and regional air quality in South of Orléans, France. J Environ Sci (China) 2024; 135:521-533. [PMID: 37778824 DOI: 10.1016/j.jes.2022.08.032] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/04/2022] [Revised: 07/14/2022] [Accepted: 08/25/2022] [Indexed: 10/03/2023]
Abstract
Wildfire events are increasing globally which may be partly associated with climate change, resulting in significant adverse impacts on local, regional air quality and global climate. In September 2020, a small wildfire (burned area: 36.3 ha) event occurred in Souesmes (Loir-et-Cher, Sologne, France), and its plume spread out over 200 km on the following day as observed by the MODIS satellite. Based on measurements at a suburban site (∼ 50 km northwest of the fire location) in Orléans and backward trajectory analysis, young wildfire plumes were characterized. Significant increases in gaseous pollutants (CO, CH4, N2O, VOCs, etc.) and particles (including black carbon) were found within the wildfire plumes, leading to a reduced air quality. Emission factors, defined as EF (X) = ∆X/∆CO (where, X represents the target species), of various trace gases and black carbon within the young wildfire plumes were determined accordingly and compared with previous studies. Changes in the ambient ions (such as ammonium, sulfate, nitrate, chloride, and nitrite in the particle- and gas- phase) and aerosol properties (e.g., aerosol water content, aerosol pH) were also quantified and discussed. Moreover, we estimated the total carbon and climate-related species (e.g., CO2, CH4, N2O, and BC) emissions and compared them with fire emission inventories. Current biomass burning emission inventories have uncertainties in estimating small fire burned areas and emissions. For instance, we found that the Global Fire Assimilation System (GFAS) may underestimate emissions (e.g., CO) of this small wildfire while other inventories (GFED and FINN) showed significant overestimation. Considering that it is the first time to record wildfire plumes in this region, related atmospheric implications are presented and discussed.
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Affiliation(s)
- Chaoyang Xue
- Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS - Université Orléans - CNES (UMR 7328), Orléans Cedex 2 45071, France
| | - Gisèle Krysztofiak
- Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS - Université Orléans - CNES (UMR 7328), Orléans Cedex 2 45071, France
| | - Yangang Ren
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France; Research Centre for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Min Cai
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France
| | - Patrick Mercier
- Lig'Air- Association de surveillance de la qualité de l'air en région Centre-Val de Loire, Saint-Cyr-en-Val 45590, France
| | - Frédéric Le Fur
- Lig'Air- Association de surveillance de la qualité de l'air en région Centre-Val de Loire, Saint-Cyr-en-Val 45590, France
| | - Corinne Robin
- Lig'Air- Association de surveillance de la qualité de l'air en région Centre-Val de Loire, Saint-Cyr-en-Val 45590, France
| | - Benoit Grosselin
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France
| | - Véronique Daële
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France
| | - Max R McGillen
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France
| | - Yujing Mu
- Research Centre for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
| | - Valéry Catoire
- Laboratoire de Physique et Chimie de l'Environnement et de l'Espace (LPC2E), CNRS - Université Orléans - CNES (UMR 7328), Orléans Cedex 2 45071, France.
| | - Abdelwahid Mellouki
- Institut de Combustion, Aérothermique, Réactivité Environnement (ICARE), CNRS, Orléans Cedex 2 45071, France; Mohammed V University, Rabat, Morocco.
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5
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Abstract
Australia rethinks strategies after 2019 to 2020 bushfires.
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Affiliation(s)
- David M J S Bowman
- Fire Centre, School of Natural Science, University of Tasmania, Hobart, Tasmania, Australia
| | - Jason J Sharples
- UNSW Bushfire Research Group, School of Science, University of New South Wales, Canberra, ACT, Australia
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6
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Benoit R, Vernier H, Vernier JP, Joly L, Dumelié N, Wienhold FG, Crevoisier C, Delpeux S, Bernard F, Dagaut P, Berthet G. The first balloon-borne sample analysis of atmospheric carbonaceous components reveals new insights into formation processes. CHEMOSPHERE 2023; 326:138421. [PMID: 36935062 DOI: 10.1016/j.chemosphere.2023.138421] [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: 11/09/2022] [Revised: 03/08/2023] [Accepted: 03/14/2023] [Indexed: 06/18/2023]
Abstract
Atmospheric aerosol optical, physical, and chemical properties play a fundamental role in the Earth's climate system. A better understanding of the processes involved in their formation, evolution, and interaction with radiation and the water cycle is critical. We report the analysis of atmospheric molecules/particles collected with a new sampling system that flew under regular weather balloons for the first time. The flight took place on January 18, 2022 from Reims (France). The samples were subsequently analyzed by high-resolution mass spectrometry (Orbitrap) to specifically infer hundreds of organic components present in 4 different layers from the troposphere to the stratosphere (up to 20 km). Additional measurements of O3, CO, and aerosol concentrations a few hours before this flight took place to contextualize the sampling. After separating common species found on each filter that might be common to atmospheric layers or residuals for contaminations, we found that each sample yields significant differences in the number and size of organic species detected that should reflect the unique composition of atmospheric layers. While tropospheric samples yield significantly oxidized and saturated components, with carbon numbers below 30 that might be explained by complex organics chemistry from local and distant source emissions, the upper tropospheric and stratospheric samples were associated with increased carbon numbers (C > 30), with a significantly reduced unsaturation number for the stratosphere, that might be induced by strong UV radiations. The multimodal distributions of carbon numbers in chemical formulas observed between 15 and 20 km suggest that oligomerization and growth of organic molecules may take place in aged air masses of tropical origin that are known to carry organic compounds even several km above the tropopause where their lifetime significantly increases. In addition, the presence of organics may also reflect the extended influence of wildfires smoke injected during the spring and summer in the NH hemisphere before the in situ observations and their long-lifetime in the upper troposphere and stratosphere.
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Affiliation(s)
| | - Hazel Vernier
- LPC2E, UMR 7328 CNRS-Université d'Orléans-CNES, Orléans, France
| | - Jean-Paul Vernier
- NASA Langley Research Center, Hampton, VA, USA; National Institute of Aerospace, Hampton, VA, USA
| | - Lilian Joly
- GSMA, UMR 7331 CNRS-Université de Reims Champagne-Ardenne, Reims, France
| | - Nicolas Dumelié
- GSMA, UMR 7331 CNRS-Université de Reims Champagne-Ardenne, Reims, France
| | | | - Cyril Crevoisier
- Laboratoire de Météorologie Dynamique (LMD/IPSL), CNRS, Ecole Polytechnique, Université Paris-Saclay, Palaiseau, France
| | | | | | | | - Gwenaël Berthet
- LPC2E, UMR 7328 CNRS-Université d'Orléans-CNES, Orléans, France
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7
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Fasullo JT, Rosenbloom N, Buchholz R. A multiyear tropical Pacific cooling response to recent Australian wildfires in CESM2. SCIENCE ADVANCES 2023; 9:eadg1213. [PMID: 37163592 PMCID: PMC10171808 DOI: 10.1126/sciadv.adg1213] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/03/2022] [Accepted: 04/06/2023] [Indexed: 05/12/2023]
Abstract
The climate response to biomass burning emissions from the 2019-2020 Australian wildfire season is estimated from two 30-member ensembles using CESM2: one of which incorporates observed wildfire emissions and one that does not. In response to the fires, an increase in biomass aerosol burdens across the southern hemisphere is simulated through late 2019 and early 2020, accompanied by an enhancement of cloud albedo, particularly in the southeastern subtropical Pacific Ocean. In turn, the surface cools, the boundary layer dries, and the moist static energy of the low-level flow into the equatorial Pacific is reduced. In response, the intertropical convergence zone migrates northward and sea surface temperature in the Niño3.4 region cools, with coupled feedbacks amplifying the cooling. A subsequent multiyear ensemble mean cooling of the tropical Pacific is simulated through the end of 2021, suggesting an important contribution to the 2020-2022 strong La Niña events.
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Affiliation(s)
| | | | - Rebecca Buchholz
- National Center for Atmospheric Research, Boulder, CO 80305, USA
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8
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Bhatta S, Pandit AK, Loughman RP, Vernier JP. Three-wavelength approach for aerosol-cloud discrimination in the SAGE III/ISS aerosol extinction dataset. APPLIED OPTICS 2023; 62:3454-3466. [PMID: 37132847 DOI: 10.1364/ao.485466] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/04/2023]
Abstract
The tropical upper troposphere and lower stratosphere (UTLS) region is dominated by aerosols and clouds affecting Earth's radiation budget and climate. Thus, satellites' continuous monitoring and identification of these layers is crucial for quantifying their radiative impact. However, distinguishing between aerosols and clouds is challenging, especially under the perturbed UTLS conditions during post-volcanic eruptions and wildfire events. Aerosol-cloud discrimination is primarily based on their disparate wavelength-dependent scattering and absorption properties. In this study, we use aerosol extinction observations in the tropical (15°N-15°S) UTLS from June 2017 to February 2021, available from the latest generation of the Stratospheric Aerosol and Gas Experiment (SAGE) instrument-SAGE III onboard the International Space Station (ISS) to study aerosols and clouds. During this period, the SAGE III/ISS provided better coverage over the tropics at additional wavelength channels (relative to previous SAGE missions) and witnessed several volcanic and wildfire events that perturbed the tropical UTLS. We explore the advantage of having an extinction coefficient at an additional wavelength channel (1550 nm) from the SAGE III/ISS in aerosol-cloud discrimination using a method based on thresholds of two extinction coefficient ratios, R 1 (520 nm/1020 nm) and R 2 (1020 nm/1550 nm). This method was proposed earlier by Kent et al. [Appl. Opt.36, 8639 (1997)APOPAI0003-693510.1364/AO.36.008639] for the SAGE III-Meteor-3M but was never tested for the tropical region under volcanically perturbed conditions. We call this method the Extinction Color Ratio (ECR) method. The ECR method is applied to the SAGE III/ISS aerosol extinction data to obtain cloud-filtered aerosol extinction coefficients, cloud-top altitude, and seasonal cloud occurrence frequency during the entire study period. Cloud-filtered aerosol extinction coefficient obtained using the ECR method revealed the presence of enhanced aerosols in the UTLS following volcanic eruptions and wildfire events consistent with the Ozone Mapping and Profiler Suite (OMPS) and space-borne lidar-Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP). The cloud-top altitude obtained from the SAGE III/ISS is within 1 km of the nearly co-located observations from OMPS and CALIOP. In general, the seasonal mean cloud-top altitude from the SAGE III/ISS events peaks during the December, January, and February months, with sunset events showing higher cloud tops than the sunrise events, indicating the seasonal and diurnal variation of the tropical convection. The seasonal altitude distribution of cloud occurrence frequency obtained from the SAGE III/ISS also agrees well with CALIOP observations within 10%. We show that the ECR method is a simple approach that relies on thresholds independent of the sampling period, providing cloud-filtered aerosol extinction coefficients uniformly for climate studies irrespective of the UTLS conditions. However, since the predecessor of SAGE III did not include a 1550 nm channel, the usefulness of this approach is limited to short-term climate studies after 2017.
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9
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Barnes PW, Robson TM, Zepp RG, Bornman JF, Jansen MAK, Ossola R, Wang QW, Robinson SA, Foereid B, Klekociuk AR, Martinez-Abaigar J, Hou WC, Mackenzie R, Paul ND. Interactive effects of changes in UV radiation and climate on terrestrial ecosystems, biogeochemical cycles, and feedbacks to the climate system. Photochem Photobiol Sci 2023; 22:1049-1091. [PMID: 36723799 PMCID: PMC9889965 DOI: 10.1007/s43630-023-00376-7] [Citation(s) in RCA: 13] [Impact Index Per Article: 13.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/22/2022] [Accepted: 01/13/2023] [Indexed: 02/02/2023]
Abstract
Terrestrial organisms and ecosystems are being exposed to new and rapidly changing combinations of solar UV radiation and other environmental factors because of ongoing changes in stratospheric ozone and climate. In this Quadrennial Assessment, we examine the interactive effects of changes in stratospheric ozone, UV radiation and climate on terrestrial ecosystems and biogeochemical cycles in the context of the Montreal Protocol. We specifically assess effects on terrestrial organisms, agriculture and food supply, biodiversity, ecosystem services and feedbacks to the climate system. Emphasis is placed on the role of extreme climate events in altering the exposure to UV radiation of organisms and ecosystems and the potential effects on biodiversity. We also address the responses of plants to increased temporal variability in solar UV radiation, the interactive effects of UV radiation and other climate change factors (e.g. drought, temperature) on crops, and the role of UV radiation in driving the breakdown of organic matter from dead plant material (i.e. litter) and biocides (pesticides and herbicides). Our assessment indicates that UV radiation and climate interact in various ways to affect the structure and function of terrestrial ecosystems, and that by protecting the ozone layer, the Montreal Protocol continues to play a vital role in maintaining healthy, diverse ecosystems on land that sustain life on Earth. Furthermore, the Montreal Protocol and its Kigali Amendment are mitigating some of the negative environmental consequences of climate change by limiting the emissions of greenhouse gases and protecting the carbon sequestration potential of vegetation and the terrestrial carbon pool.
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Affiliation(s)
- P W Barnes
- Biological Sciences and Environment Program, Loyola University New Orleans, New Orleans, USA.
| | - T M Robson
- Organismal & Evolutionary Biology (OEB), Faculty of Biological and Environmental Sciences, Viikki Plant Sciences Centre (ViPS), University of Helsinki, Helsinki, Finland.
- National School of Forestry, University of Cumbria, Ambleside, UK.
| | - R G Zepp
- ORD/CEMM, US Environmental Protection Agency, Athens, GA, USA
| | - J F Bornman
- Food Futures Institute, Murdoch University, Perth, Australia
| | | | - R Ossola
- Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, USA
| | - Q-W Wang
- Institute of Applied Ecology, Chinese Academy of Sciences (CAS), Shenyang, China
| | - S A Robinson
- Global Challenges Program & School of Earth, Atmospheric and Life Sciences, Securing Antarctica's Environmental Future, University of Wollongong, Wollongong, Australia
| | - B Foereid
- Environment and Natural Resources, Norwegian Institute of Bioeconomy Research, Ås, Norway
| | - A R Klekociuk
- Antarctic Climate Program, Australian Antarctic Division, Kingston, Australia
| | - J Martinez-Abaigar
- Faculty of Science and Technology, University of La Rioja, Logroño (La Rioja), Spain
| | - W-C Hou
- Department of Environmental Engineering, National Cheng Kung University, Tainan City, Taiwan
| | - R Mackenzie
- Cape Horn International Center (CHIC), Puerto Williams, Chile
- Millennium Institute Biodiversity of Antarctic and Subantarctic Ecosystems (BASE), Santiago, Chile
| | - N D Paul
- Lancaster Environment Centre, Lancaster University, Lancaster, UK
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10
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Hong X, Liu C, Zhang C, Tian Y, Wu H, Yin H, Zhu Y, Cheng Y. Vast ecosystem disturbance in a warming climate may jeopardize our climate goal of reducing CO 2: a case study for megafires in the Australian 'black summer'. THE SCIENCE OF THE TOTAL ENVIRONMENT 2023; 866:161387. [PMID: 36621492 DOI: 10.1016/j.scitotenv.2023.161387] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/24/2022] [Revised: 12/31/2022] [Accepted: 01/01/2023] [Indexed: 06/17/2023]
Abstract
A warming climate is one of the most important driving forces of intensified wildfires globally. The unprecedented wildfires broke out in the Australian 'Black Summer' (November 2019-February 2020), which released massive heat, gases, and particles into the atmosphere. The total carbon dioxide (CO2) emissions from wildfires were estimated at ∼963 million tons by using a top-down approach based on direct satellite measurements of CO2 and fire radiative power. The fire emissions have led to an approximately 50-80 folds increase in total CO2 emission in Australia compared with the similar seasons of 2014-2019. The excess CO2 from wildfires has offset almost half of the global anthropogenic CO2 emission reductions due to the Corona Virus Disease 2019 in 2020. When the wildfires were intense in December 2019, they caused a 1.48 watts per square meter additional positive radiative forcing above the monthly average in Australia and the vicinity. Our findings demonstrate that vast ecosystem disturbance in a warming climate can strongly influence the global carbon cycle and hamper our climate goal of reducing CO2.
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Affiliation(s)
- Xinhua Hong
- School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230026, China
| | - Cheng Liu
- Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei 230026, China; Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; Anhui Institute of Optics and Fine Mechanics, HFIPS, Chinese Academy of Sciences, Hefei 230031, China.
| | - Chengxin Zhang
- Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei 230026, China
| | - Yuan Tian
- Information Materials and Intelligent Sensing Laboratory of Anhui Province, Hefei 230031, China; Institutes of Physical Science and Information Technology, Anhui University, Hefei 230031, China
| | - Hongyu Wu
- School of Environmental Science and Optoelectronic Technology, University of Science and Technology of China, Hefei 230026, China
| | - Hao Yin
- Anhui Institute of Optics and Fine Mechanics, HFIPS, Chinese Academy of Sciences, Hefei 230031, China
| | - Yizhi Zhu
- Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Chinese Academy of Sciences, Hefei 230031, China
| | - Yafang Cheng
- Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei 230026, China; Minerva Research Group, Max Planck Institute for Chemistry, Mainz 55128, Germany.
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11
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Optical observations of thunderstorms from the International Space Station: recent results and perspectives. NPJ Microgravity 2023; 9:12. [PMID: 36739448 PMCID: PMC9899213 DOI: 10.1038/s41526-023-00257-4] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/11/2022] [Accepted: 01/20/2023] [Indexed: 02/06/2023] Open
Abstract
The International Space Station (ISS) is in the lowest available orbit at ~400 km altitude, bringing instruments as close to the atmosphere as possible from the vantage point of space. The orbit inclination is 51.6°, which brings the ISS over all the low- and mid-latitude regions of the Earth and at all local times. It is an ideal platform to observe deep convection and electrification of thunderstorms, taken advantage of by the Lightning Imaging Sensor (LIS) and the Atmosphere Space Interaction Monitor (ASIM) experiments. In the coming years, meteorological satellites in geostationary orbit (~36,000 km altitude) will provide sophisticated cloud and lightning observations with almost complete coverage of the Earth's thunderstorm regions. In addition, Earth-observing satellite instruments in geostationary- and low-Earth orbit (LEO) will measure more atmospheric parameters at a higher resolution than we know today. The new infrastructure in space offers an opportunity to advance our understanding of the role of thunderstorms in atmospheric dynamics and climate change. Here, we discuss how observations from the ISS or other LEO platforms with instruments that view the atmosphere at slanted angles can complement the measurements from primarily nadir-oriented instruments of present and planned missions. We suggest that the slanted viewing geometry from LEO may resolve the altitude of electrical activity and the cloud structure where they occur, with implications for modelling thunderstorms' effects on the atmosphere's radiative properties and climate balance.
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Yang H, Gladich I, Boucly A, Artiglia L, Ammann M. Orcinol and resorcinol induce local ordering of water molecules near the liquid-vapor interface. ENVIRONMENTAL SCIENCE: ATMOSPHERES 2022; 2:1277-1291. [PMID: 36561553 PMCID: PMC9648629 DOI: 10.1039/d2ea00015f] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 03/02/2022] [Accepted: 08/17/2022] [Indexed: 12/25/2022]
Abstract
Resorcinol and orcinol are simple members of the family of phenolic compounds present in particulate matter in the atmosphere; they are amphiphilic in nature and thus surface active in aqueous solution. Here, we used X-ray photoelectron spectroscopy to probe the concentration of resorcinol (benzene-1,3-diol) and orcinol (5-methylbenzene-1,3-diol) at the liquid-vapor interface of aqueous solutions. Qualitatively consistent surface propensity and preferential orientation was obtained by molecular dynamics simulations. Auger electron yield near-edge X-ray absorption fine structure (NEXAFS) spectroscopy was used to probe the hydrogen bonding (HB) structure, indicating that the local structure of water molecules near the surface of the resorcinol and orcinol solutions tends towards a larger fraction of tetrahedrally coordinated molecules than observed at the liquid-vapor interface of pure water. The order parameter obtained from the molecular dynamics simulations confirm these observations. This effect is being discussed in terms of the formation of an ordered structure of these molecules at the surface leading to patterns of hydrated OH groups with distances among them that are relatively close to those in ice. These results suggest that the self-assembly of phenolic species at the aqueous solution-air interface could induce freezing similar to the case of fatty alcohol monolayers and, thus, be of relevance for ice nucleation in the atmosphere. We also attempted at looking at the changes of the O 1b1, 3a2 and 1b2 molecular orbitals of liquid water, which are known to be sensitive to the HB structure as well, in response to the presence of resorcinol and orcinol. However, these changes remained negligible within uncertainty for both experimentally obtained valence spectra and theoretically calculated density of states.
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Affiliation(s)
- Huanyu Yang
- Laboratory of Environmental Chemistry, Paul Scherrer Institut5232 VilligenSwitzerland,Institute of Atmospheric and Climate Science, ETH Zürich8092 ZürichSwitzerland
| | - Ivan Gladich
- Qatar Environment & Energy Research Institute, Hamad Bin Khalifa UniversityP.O. Box 34110DohaQatar
| | - Anthony Boucly
- Laboratory of Environmental Chemistry, Paul Scherrer Institut5232 VilligenSwitzerland,Electrochemistry Laboratory, Paul Scherrer Institut5232 VilligenSwitzerland
| | - Luca Artiglia
- Laboratory of Environmental Chemistry, Paul Scherrer Institut5232 VilligenSwitzerland,Laboratory for Catalysis and Sustainable Chemistry, Paul Scherrer Institut5232 VilligenSwitzerland
| | - Markus Ammann
- Laboratory of Environmental Chemistry, Paul Scherrer Institut5232 VilligenSwitzerland
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Diamond MS, Gristey JJ, Kay JE, Feingold G. Anthropogenic aerosol and cryosphere changes drive Earth's strong but transient clear-sky hemispheric albedo asymmetry. COMMUNICATIONS EARTH & ENVIRONMENT 2022; 3:206. [PMID: 36118252 PMCID: PMC9466336 DOI: 10.1038/s43247-022-00546-y] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 05/06/2022] [Accepted: 08/31/2022] [Indexed: 06/15/2023]
Abstract
A striking feature of the Earth system is that the Northern and Southern Hemispheres reflect identical amounts of sunlight. This hemispheric albedo symmetry comprises two asymmetries: The Northern Hemisphere is more reflective in clear skies, whereas the Southern Hemisphere is cloudier. Here we show that the hemispheric reflection contrast from differences in continental coverage is offset by greater reflection from the Antarctic than the Arctic, allowing the net clear-sky asymmetry to be dominated by aerosol. Climate model simulations suggest that historical anthropogenic aerosol emissions drove a large increase in the clear-sky asymmetry that would reverse in future low-emission scenarios. High-emission scenarios also show decreasing asymmetry, instead driven by declines in Northern Hemisphere ice and snow cover. Strong clear-sky hemispheric albedo asymmetry is therefore a transient feature of Earth's climate. If all-sky symmetry is maintained, compensating cloud changes would have uncertain but important implications for Earth's energy balance and hydrological cycle.
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Affiliation(s)
- Michael S. Diamond
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309 USA
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305 USA
| | - Jake J. Gristey
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309 USA
- NOAA Chemical Sciences Laboratory, Boulder, CO 80305 USA
- Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO 80303 USA
| | - Jennifer E. Kay
- Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309 USA
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Australian wildfires cause the largest stratospheric warming since Pinatubo and extends the lifetime of the Antarctic ozone hole. Sci Rep 2022; 12:12665. [PMID: 36008428 PMCID: PMC9411169 DOI: 10.1038/s41598-022-15794-3] [Citation(s) in RCA: 6] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/24/2022] [Accepted: 06/29/2022] [Indexed: 11/09/2022] Open
Abstract
Global mean lower stratosphere temperatures rose abruptly in January 2020 reaching values not experienced since the early 1990s. Anomalously high lower stratospheric temperatures were recorded for 4 months at highly statistically significant levels. Here, we use a combination of satellite and surface-based remote sensing observations to derive a time-series of stratospheric biomass burning aerosol optical depths originating from intense SouthEastern Australian wildfires and use these aerosol optical depths in a state-of-the-art climate model. We show that the S.E. Australian wildfires are the cause of this lower stratospheric warming. We also investigate the radiatively-driven dynamical response to the observed stratospheric ozone perturbation and find a significant strengthening of the springtime Antarctic polar vortex suggesting that biomass burning aerosols play a significant role in the observed anomalous longevity of the ozone hole in 2020.
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A Lightweight CNN Model Based on GhostNet. COMPUTATIONAL INTELLIGENCE AND NEUROSCIENCE 2022; 2022:8396550. [PMID: 35958795 PMCID: PMC9357762 DOI: 10.1155/2022/8396550] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 06/02/2022] [Accepted: 07/09/2022] [Indexed: 11/18/2022]
Abstract
The existing deep learning models have problems such as large weight parameters and slow inference speed of equipment. In practical applications such as fire detection, they often cannot be deployed on equipment with limited resources due to the huge amount of parameters and low efficiency. In response to this problem, this paper proposes a lightweight smoke detection model based on the convolutional attention mechanism module. The model is based on the YOLOv5 lightweight framework. The backbone network draws on the GhostNet design idea, replaces the CSP structure of the FPN and head layers with the GhostBottleNeck module, adds a convolutional attention mechanism module to the backbone network layer, and uses the CIoU loss function to improve the regression accuracy. Using YOLOv5s as the benchmark model, the parameter amount of the proposed lightweight neural network model is 2.75 M, and the floating-point calculation amount is 2.56 G, which is much lower than the parameter amount and calculation amount of the benchmark model. Tested on the public fire dataset, compared with the traditional deep learning algorithm, the model proposed in the paper has better detection performance and the detection speed is significantly better than the benchmark model. Tested under the unquantized simulator, the speed of the proposed model to detect a single picture is 60 ms, which can meet the requirements of real-time engineering applications.
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Millán L, Santee ML, Lambert A, Livesey NJ, Werner F, Schwartz MJ, Pumphrey HC, Manney GL, Wang Y, Su H, Wu L, Read WG, Froidevaux L. The Hunga Tonga-Hunga Ha'apai Hydration of the Stratosphere. GEOPHYSICAL RESEARCH LETTERS 2022; 49:e2022GL099381. [PMID: 35865735 DOI: 10.1029/2021gl096270] [Citation(s) in RCA: 6] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/30/2022] [Revised: 05/31/2022] [Accepted: 06/02/2022] [Indexed: 05/21/2023]
Abstract
Following the 15 January 2022 Hunga Tonga-Hunga Ha'apai eruption, several trace gases measured by the Aura Microwave Limb Sounder (MLS) displayed anomalous stratospheric values. Trajectories and radiance simulations confirm that the H2O, SO2, and HCl enhancements were injected by the eruption. In comparison with those from previous eruptions, the SO2 and HCl mass injections were unexceptional, although they reached higher altitudes. In contrast, the H2O injection was unprecedented in both magnitude (far exceeding any previous values in the 17-year MLS record) and altitude (penetrating into the mesosphere). We estimate the mass of H2O injected into the stratosphere to be 146 ± 5 Tg, or ∼10% of the stratospheric burden. It may take several years for the H2O plume to dissipate. This eruption could impact climate not through surface cooling due to sulfate aerosols, but rather through surface warming due to the radiative forcing from the excess stratospheric H2O.
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Affiliation(s)
- L Millán
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - M L Santee
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - A Lambert
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - N J Livesey
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - F Werner
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - M J Schwartz
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - H C Pumphrey
- School of GeoSciences The University of Edinburgh Edinburgh UK
| | - G L Manney
- NorthWest Research Associates Socorro NM USA
- New Mexico Institute of Mining and Technology Socorro NM USA
| | - Y Wang
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
- Division of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA
| | - H Su
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - L Wu
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - W G Read
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
| | - L Froidevaux
- Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA
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Shuman JK, Balch JK, Barnes RT, Higuera PE, Roos CI, Schwilk DW, Stavros EN, Banerjee T, Bela MM, Bendix J, Bertolino S, Bililign S, Bladon KD, Brando P, Breidenthal RE, Buma B, Calhoun D, Carvalho LMV, Cattau ME, Cawley KM, Chandra S, Chipman ML, Cobian-Iñiguez J, Conlisk E, Coop JD, Cullen A, Davis KT, Dayalu A, De Sales F, Dolman M, Ellsworth LM, Franklin S, Guiterman CH, Hamilton M, Hanan EJ, Hansen WD, Hantson S, Harvey BJ, Holz A, Huang T, Hurteau MD, Ilangakoon NT, Jennings M, Jones C, Klimaszewski-Patterson A, Kobziar LN, Kominoski J, Kosovic B, Krawchuk MA, Laris P, Leonard J, Loria-Salazar SM, Lucash M, Mahmoud H, Margolis E, Maxwell T, McCarty JL, McWethy DB, Meyer RS, Miesel JR, Moser WK, Nagy RC, Niyogi D, Palmer HM, Pellegrini A, Poulter B, Robertson K, Rocha AV, Sadegh M, Santos F, Scordo F, Sexton JO, Sharma AS, Smith AMS, Soja AJ, Still C, Swetnam T, Syphard AD, Tingley MW, Tohidi A, Trugman AT, Turetsky M, Varner JM, Wang Y, Whitman T, Yelenik S, Zhang X. Reimagine fire science for the anthropocene. PNAS NEXUS 2022; 1:pgac115. [PMID: 36741468 PMCID: PMC9896919 DOI: 10.1093/pnasnexus/pgac115] [Citation(s) in RCA: 2] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/13/2021] [Accepted: 08/02/2022] [Indexed: 02/07/2023]
Abstract
Fire is an integral component of ecosystems globally and a tool that humans have harnessed for millennia. Altered fire regimes are a fundamental cause and consequence of global change, impacting people and the biophysical systems on which they depend. As part of the newly emerging Anthropocene, marked by human-caused climate change and radical changes to ecosystems, fire danger is increasing, and fires are having increasingly devastating impacts on human health, infrastructure, and ecosystem services. Increasing fire danger is a vexing problem that requires deep transdisciplinary, trans-sector, and inclusive partnerships to address. Here, we outline barriers and opportunities in the next generation of fire science and provide guidance for investment in future research. We synthesize insights needed to better address the long-standing challenges of innovation across disciplines to (i) promote coordinated research efforts; (ii) embrace different ways of knowing and knowledge generation; (iii) promote exploration of fundamental science; (iv) capitalize on the "firehose" of data for societal benefit; and (v) integrate human and natural systems into models across multiple scales. Fire science is thus at a critical transitional moment. We need to shift from observation and modeled representations of varying components of climate, people, vegetation, and fire to more integrative and predictive approaches that support pathways toward mitigating and adapting to our increasingly flammable world, including the utilization of fire for human safety and benefit. Only through overcoming institutional silos and accessing knowledge across diverse communities can we effectively undertake research that improves outcomes in our more fiery future.
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Affiliation(s)
- Jacquelyn K Shuman
- Terrestrial Sciences Section, Climate and Global Dynamics Laboratory, National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307-3000, USA
| | - Jennifer K Balch
- Earth Lab, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder,4001 Discovery Drive, Suite S348 611 UCB, Boulder, CO, 80303, USA
| | - Rebecca T Barnes
- Environmental Studies Program, Colorado College, 14 East Cache la Poudre, Colorado Springs, CO, 80903, USA
| | - Philip E Higuera
- Department of Ecosystem and Conservation Sciences, University of Montana, 32 Campus Dr., Missoula, MT, 59812, USA
| | - Christopher I Roos
- Department of Anthropology, Southern Methodist University, P.O. Box 750336, Dallas, TX, 75275-0336, USA
| | - Dylan W Schwilk
- Department of Biological Sciences, Texas Tech University, 2901 Main St. Lubbock, TX, 79409-43131, USA
| | - E Natasha Stavros
- Earth Lab, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder,4001 Discovery Drive, Suite S348 611 UCB, Boulder, CO, 80303, USA
| | - Tirtha Banerjee
- Samueli School of Engineering, University of California, 3084 Interdisciplinary Science and Engineering Building, UC Irvine, CA 92697, USA
| | - Megan M Bela
- Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado at Boulder, 216 UCB, Boulder CO, 80309, USA
- NOAA Chemical Sciences Laboratory, Boulder, CO, USA
| | - Jacob Bendix
- Department of Geography and the Environment, Syracuse University, 144 Eggers Hall, Syracuse NY 13244, USA
| | - Sandro Bertolino
- Department of Life Sciences and Systems Biology, University of Turin, Via Accademia Albertina 13, 10123 Torino, Italy
| | - Solomon Bililign
- Department of Physics, North Carolina A&T State University, 1601 E Market Street, Greensboro, NC 27411, USA
| | - Kevin D Bladon
- Department of Forest Engineering, Resources, and Management, Oregon State University, 244 Peavy Forest Science Center; Corvallis, OR, 97331, USA
| | - Paulo Brando
- Earth System Science, University of California Irvine, 3215 Croul Hall Irvine, CA 92697, USA
| | - Robert E Breidenthal
- Department of Aeronautics and Astronautics, University of Washington, Box 352400, Seattle, WA 98195-2400, USA
| | - Brian Buma
- Integrative Biology, University of Colorado Denver, Campus Box 171, P.O. Box 173364, Denver, CO 80217-3364, USA
| | - Donna Calhoun
- Department of Mathematics, Boise State University, 1910 University Drive, Boise, ID 83725-1135, USA
| | - Leila M V Carvalho
- Department of Geography, University of California Santa Barbara, 1832 Ellison Hall, Santa Barbara, CA, 93106, USA
| | - Megan E Cattau
- Human-Environment Systems, Boise State University, Boise State Environmental Research Building, 1295 W University Dr, Boise, ID 83706, USA
| | - Kaelin M Cawley
- National Ecological Observatory Network, Battelle, 1685 38th St., Suite 100, Boulder, CO 80301, USA
| | - Sudeep Chandra
- Global Water Center, University of Nevada, 1664 N. Virginia, Reno, NV, 89509, USA
| | - Melissa L Chipman
- Department of Earth and Environmental Sciences, Syracuse University, 317 Heroy Geology Building, 141 Crouse Dr, Syracuse, NY 13210, USA
| | - Jeanette Cobian-Iñiguez
- Department of Mechanical Engineering, University of California Merced, Sustainability Research and Engineering, SRE 366, 5200 Lake Rd, Merced, CA 95343, USA
| | - Erin Conlisk
- Point Blue Conservation Science, 3820 Cypress Dr, Petaluma, CA 94954, USA
| | - Jonathan D Coop
- Clark School of Environment and Sustainability, Western Colorado University, 1 Western Way, Gunnison CO 81231, USA
| | - Alison Cullen
- Evans School of Public Policy and Governance, University of Washington, Parrington Hall, Mailbox 353055, Seattle, WA 98195-3055, USA
| | - Kimberley T Davis
- Department of Ecosystem and Conservation Sciences, University of Montana, 32 Campus Dr., Missoula, MT, 59812, USA
| | - Archana Dayalu
- Atmospheric and Environmental Research, 131 Hartwell Ave, Lexington MA 02421, USA
| | - Fernando De Sales
- Department of Geography, San Diego State University, 5500 Campanile Drive, San Diego, CA 92182-4493, USA
| | - Megan Dolman
- Human-Environment Systems, Boise State University, Boise State Environmental Research Building, 1295 W University Dr, Boise, ID 83706, USA
| | - Lisa M Ellsworth
- Department of Fisheries, Wildlife, and Conservation Sciences, Oregon State University, 104 Nash Hall, Corvallis, OR 97330, USA
| | - Scott Franklin
- School of Biological Sciences, University of Northern Colorado, 501 20th Street, Greeley, CO 80639, USA
| | - Christopher H Guiterman
- Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado at Boulder, 216 UCB, Boulder CO, 80309, USA
- NOAA's National Centers for Environmental Information (NCEI), 325 Broadway, NOAA E/GC3, Boulder, Colorado 80305-3337, USA
| | - Matthew Hamilton
- School of Environment and Natural Resources, The Ohio State University, 2021 Coffey Road, Columbus, OH 43210, USA
| | - Erin J Hanan
- Department of Natural Resources and Environmental Science, University of Nevada, 1664 N. Virginia St. Mail Stop 0186. Reno, NV 89509, USA
| | - Winslow D Hansen
- Cary Institute of Ecosystem Studies, PO Box AB, Millbrook, NY 12545, USA
| | - Stijn Hantson
- Earth System Science Program, Faculty of Natural Sciences, Max Planck Tandem Group in Earth System Science, Universidad del Rosario, Carrera 26 # 63b-48, Bogota, DC 111221, Colombia
| | - Brian J Harvey
- School of Environmental and Forest Sciences, University of Washington, UW-SEFS, Box 352100, Seattle, WA 98195, USA
| | - Andrés Holz
- Department of Geography, Portland State University, 1721 SW Broadway, Portland, OR 97201, USA
| | - Tao Huang
- Human-Environment Systems, Boise State University, Boise State Environmental Research Building, 1295 W University Dr, Boise, ID 83706, USA
| | - Matthew D Hurteau
- Department of Biology, University of New Mexico, MSC03 2020, Albuquerque, NM 87131, USA
| | - Nayani T Ilangakoon
- Earth Lab, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder,4001 Discovery Drive, Suite S348 611 UCB, Boulder, CO, 80303, USA
| | - Megan Jennings
- Institute for Ecological Monitoring and Management, San Diego State University, 5500 Campanile Drive, San Diego, CA 92182-4614, USA
| | - Charles Jones
- Department of Geography, University of California Santa Barbara, 1832 Ellison Hall, Santa Barbara, CA, 93106, USA
| | | | - Leda N Kobziar
- College of Natural Resources, University of Idaho, 1031 N. Academic Way Coeur d'Alene, ID 83844, USA
| | - John Kominoski
- Institute of Environment and Department of Biological Sciences, Florida International University, 11200 SW 8th Street, Miami, FL, 33199, USA
| | - Branko Kosovic
- Weather Systems and Assessment Program, National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307-3000, USA
| | - Meg A Krawchuk
- Department of Forest Ecosystems and Society, Oregon State University, Richardson Hall, Corvallis, OR 97331, USA
| | - Paul Laris
- Department of Geography, California State University Long Beach, Long Beach, 1250 Bellflower Blvd, Long Beach, CA 90840, USA
| | - Jackson Leonard
- Rocky Mountain Research Station, U.S.D.A. Forest Service, 2500 S. Pine Knoll Dr. Flagstaff, Arizona 86001, USA
| | | | - Melissa Lucash
- Department of Geography, University of Oregon, 1251 University of Oregon, Eugene OR 97403-1251, USA
| | - Hussam Mahmoud
- Department of Civil and Environmental Engineering, Colorado State University, 1372 Campus Delivery, Fort Collins, CO, 80523, USA
| | - Ellis Margolis
- U.S. Geological Survey, Fort Collins Science Center, New Mexico Landscapes Field Station, 15 Entrance Rd., Los Alamos, NM 87544, USA
| | - Toby Maxwell
- Department of Biological Sciences, Boise State University, 1910 University Dr. Boise ID 83725, USA
| | - Jessica L McCarty
- Department of Geography and Geospatial Analysis Center, Miami University, 217 Shideler Hall, Oxford, OH 45056, USA
| | - David B McWethy
- Department of Earth Sciences, Montana State University, 226 Traphagen Hall, Bozeman, MT 59717, USA
| | - Rachel S Meyer
- Department of Ecology and Evolutionary Biology, University of California Santa Cruz, 130 McAllister Way, Santa Cruz, CA 95060, USA
| | - Jessica R Miesel
- Department of Plant, Soil and Microbial Sciences, Michigan State University, 1066 Bogue Street Rm A286, East Lansing, MI 48823, USA
| | - W Keith Moser
- Rocky Mountain Research Station, U.S.D.A. Forest Service, 2500 S. Pine Knoll Dr. Flagstaff, Arizona 86001, USA
| | - R Chelsea Nagy
- Earth Lab, Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado Boulder,4001 Discovery Drive, Suite S348 611 UCB, Boulder, CO, 80303, USA
| | - Dev Niyogi
- Jackson School of Geosciences, and Cockrell School of Engineering, University of Texas at Austin, 2305 Speedway Stop C1160, Austin, TX 78712-1692, USA
| | - Hannah M Palmer
- Department of Life and Environmental Sciences, University of California Merced, Merced, 5200 Lake Rd, Merced, CA 95343, USA
| | - Adam Pellegrini
- Department of Plant Sciences, University of Cambridge, Downing St, Cambridge, CB2 3EA, UK
| | - Benjamin Poulter
- NASA Goddard Space Flight Center, Greenbelt Road, Greenbelt, MD 20771, USA
| | - Kevin Robertson
- Tall Timbers Research Station and Land Conservancy, 13093 Henry Beadel Drive, Tallahassee, FL 32312, USA
| | - Adrian V Rocha
- Department of Biological Sciences, University of Notre Dame, 100 Campus Dr., Notre Dame, IN 46556, USA
| | - Mojtaba Sadegh
- Department of Civil Engineering, Boise State University, 1910 University Drive, Boise, ID, 83725, USA
| | - Fernanda Santos
- Environmental Sciences Division, Oak Ridge National Laboratory, One Bethel Valley Road, P.O. Box 2008, MS-6038, Oak Ridge, TN 37831-6038, USA
| | - Facundo Scordo
- Global Water Center and the Department of Biology, University of Nevada, 1664 N. Virginia, Reno, NV, 89509, USA
- Instituto Argentino de Oceanografía (IADO-CONICET-UNS), Florida 8000, Bahía Blanca, B8000BFW Buenos Aires, Argentina
| | - Joseph O Sexton
- terraPulse, Inc., 13201 Squires Ct., North Potomac, MD 20878, USA
| | - A Surjalal Sharma
- Department of Astronomy, University of Maryland, 4296 Stadium Dr., Astronomy Dept Room 1113, College Park, MD 20742, USA
| | - Alistair M S Smith
- Department of Earth and Spatial Sciences, College of Science, University of Idaho, 875 Perimeter Drive MS 3021, Moscow ID, 83843-3021, USA
- Department of Forest, Rangeland, and Fire Science, College of Natural Resources, University of Idaho, 875 Perimeter Drive MS 1133, Moscow, ID 83844-1133, USA
| | - Amber J Soja
- NASA Langley Research Center, NASA, 2 Langley Blvd, Hampton, VA 23681, USA
- National Institute of Aerospace, NASA, 100 Exploration Way, Hampton, VA 23666, USA
| | - Christopher Still
- Department of Forest Ecosystems and Society, Oregon State University, Richardson Hall, Corvallis, OR 97331, USA
| | - Tyson Swetnam
- Data Science Institute, University of Arizona, 1657 E Helen St, Tucson, AZ 85721, USA
| | - Alexandra D Syphard
- Conservation Biology Institute, 10423 Sierra Vista Ave., La Mesa, CA, 91941, USA
| | - Morgan W Tingley
- Ecology and Evolutionary Biology, University of California Los Angeles, 621 Charles E Young Dr S #951606, Los Angeles, CA 90095, USA
| | - Ali Tohidi
- Department of Mechanical Engineering, San Jose State University, Room 310-K, ENG Building, 1 Washington Square, San Jose, CA 95112, USA
| | - Anna T Trugman
- Department of Geography, University of California Santa Barbara, 1832 Ellison Hall, Santa Barbara, CA, 93106, USA
| | - Merritt Turetsky
- Institute of Arctic and Alpine Research, University of Colorado Boulder, Campus Box 450, Boulder, CO 80309-0450, USA
| | - J Morgan Varner
- Tall Timbers Research Station and Land Conservancy, 13093 Henry Beadel Drive, Tallahassee, FL 32312, USA
| | - Yuhang Wang
- School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30332, USA
| | - Thea Whitman
- Department of Soil Science, University of Wisconsin-Madison, 1525 Observatory Dr., Madison, WI 53711, USA
| | - Stephanie Yelenik
- Rocky Mountain Research Station, U.S.D.A. Forest Service, 920 Valley Road, Reno NV, 89512, USA
| | - Xuan Zhang
- Department of Life and Environmental Sciences, University of California Merced, Merced, 5200 Lake Rd, Merced, CA 95343, USA
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18
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Australian Bushfires (2019–2020): Aerosol Optical Properties and Radiative Forcing. ATMOSPHERE 2022. [DOI: 10.3390/atmos13060867] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 11/16/2022]
Abstract
In the present study, we present the aerosol optical properties and radiative forcing (RF) of the tropospheric and stratospheric smoke layers, observed by the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) satellite, during the extraordinary Australian biomass burning (BB) event in 2019–2020. These BB layers were studied and analyzed within the longitude range 140° E–20° W and the latitude band 20°–60° S, as they were gradually transported from the Australian banks to the South American continent. These layers were found to be trapped within the Andes circulation, staying for longer time periods in the same longitude region. The BB aerosols reached altitudes even up to 22 km amsl., and regarding their optical properties, they were found to be nearly spherical (particle linear depolarization ratio (PLDR) < 0.10) in the troposphere; while, in the stratosphere, they were more depolarizing with PLDR values reaching up to 0.20. Fine and ultrafine smoke particles were dominant in the stratosphere, according to the observed Ångström exponent, related to the backscatter coefficients obtained by the pair of wavelengths 532 and 1064 nm (Åb up to 3), in contrast to the Åb values in the troposphere (Åb < 1) indicative of the presence of coarser particles. As the aerosols fend off the source, towards North America, a slightly descending trend was observed in the tropospheric Åb values, while the stratospheric ones were lightly increased. A maximum aerosol optical depth (AOD) value of 0.54 was recorded in the lower troposphere over the fire spots, while, in the stratosphere, AOD values up to 0.29 were observed. Sharp changes of carbon monoxide (CO) and ozone (O3) concentrations were also recorded by the Copernicus Atmosphere Monitoring Service (CAMS) in various atmospheric heights over the study region, associated with fire smoke emissions. The tropospheric smoke layers were found to have a negative mean radiative effect, ranging from −12.83 W/m2 at the top of the atmosphere (TOA), to −32.22 W/m2 on the surface (SRF), while the radiative effect of the stratospheric smoke was estimated between −7.36 at the TOA to −18.51 W/m2 at the SRF.
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Wang Y, Chen HH, Tang R, He D, Lee Z, Xue H, Wells M, Boss E, Chai F. Australian fire nourishes ocean phytoplankton bloom. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 807:150775. [PMID: 34619187 DOI: 10.1016/j.scitotenv.2021.150775] [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: 07/04/2021] [Revised: 09/17/2021] [Accepted: 09/17/2021] [Indexed: 06/13/2023]
Abstract
An unprecedented devastating forest fire occurred in Australia from September 2019 to March 2020. Satellite observations revealed that this rare fire event in Australia destroyed a record amount of more than 202,387 km2 of forest, including 56,471 km2 in eastern Australia, which is mostly composed of evergreen forest. The released aerosols contained essential nutrients for the growth of marine phytoplankton and were transported by westerly winds over the Southern Ocean, with rainfall-induced deposition to the ocean beneath. Here, we show that a prominent oceanic bloom, indicated by the rapid growth of phytoplankton, took place in the Southern Ocean along the trajectory of fire-born aerosols in response to atmospheric deposition. Calculations of carbon released during the fire versus carbon absorbed by the oceanic phytoplankton bloom suggest that they were nearly equal. This finding illustrates the critical role of the oceans in mitigating natural and anthropogenic carbon dioxide releases to the atmosphere, which are a primary driver of climate change.
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Affiliation(s)
- Yuntao Wang
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Huan-Huan Chen
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; Ocean College, Zhejiang University, Zhoushan 316021, China
| | - Rui Tang
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Ding He
- Department of Ocean Science and Hong Kong Branch of the Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), The Hong Kong University of Science and Technology, Hong Kong, China; Organic Geochemistry Unit, School of Earth Sciences, Zhejiang University, Hangzhou 310027, China
| | - Zhongping Lee
- School for the Environment, University of Massachusetts Boston, Boston 02125, USA
| | - Huijie Xue
- State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361102, China; College of Ocean and Earth Sciences, Xiamen University, Xiamen 361102, China
| | - Mark Wells
- School of Marine Sciences, University of Maine, Orono 04469, USA; State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
| | - Emmanuel Boss
- School of Marine Sciences, University of Maine, Orono 04469, USA
| | - Fei Chai
- State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; Ocean College, Zhejiang University, Zhoushan 316021, China.
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Fang Z, Li C, He Q, Czech H, Gröger T, Zeng J, Fang H, Xiao S, Pardo M, Hartner E, Meidan D, Wang X, Zimmermann R, Laskin A, Rudich Y. Secondary organic aerosols produced from photochemical oxidation of secondarily evaporated biomass burning organic gases: Chemical composition, toxicity, optical properties, and climate effect. ENVIRONMENT INTERNATIONAL 2021; 157:106801. [PMID: 34343933 DOI: 10.1016/j.envint.2021.106801] [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: 05/20/2021] [Revised: 06/29/2021] [Accepted: 07/26/2021] [Indexed: 06/13/2023]
Abstract
Biomass burning (BB) is an important source of primary organic aerosols (POA). These POA contain a significant fraction of semivolatile organic compounds, and can release them into the gas phase during the dilution process in transport. Such evaporated compounds were termed "secondarily evaporated BB organic gases (SBB-OGs)" to distinguish them from the more studied primary emissions. SBB-OGs contribute to the formation of secondary organic aerosols (SOA) through reactions with atmospheric oxidants, and thus may influence human health and the Earth's radiation budget. In this study, tar materials collected from wood pyrolysis were taken as proxies for POA from smoldering-phase BB and were used to release SBB-OGs constantly in the lab. OH-initiated oxidation of the SBB-OGs in the absence of NOx was investigated using an oxidation flow reactor, and the chemical, optical, and toxicological properties of SOA were comprehensively characterized. Carbonyl compounds were the most abundant species in identified SOA species. Human lung epithelial cells exposed to an environmentally relevant dose of the most aged SOA did not exhibit detectable cell mortality. The oxidative potential of SOA was characterized with the dithiothreitol (DTT) assay, and its DTT consumption rate was 15.5 ± 0.5 pmol min-1 μg-1. The SOA present comparable light scattering to BB-POA, but have lower light absorption with imaginary refractive index less than 0.01 within the wavelength range of 360-600 nm. Calculations based on Mie theory show that pure airborne SOA with atmospherically relevant sizes of 50-400 nm have a cooling effect; when acting as the coating materials, these SOA can counteract the warming effect brought by airborne black carbon aerosol.
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Affiliation(s)
- Zheng Fang
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - Chunlin Li
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - Quanfu He
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - Hendryk Czech
- Joint Mass Spectrometry Centre, Chair of Analytical Chemistry, Institute of Chemistry, University of Rostock, 18059 Rostock, Germany; Joint Mass Spectrometry Centre, Comprehensive Molecular Analytics, Helmholtz Zentrum München, 81379 München, Germany
| | - Thomas Gröger
- Joint Mass Spectrometry Centre, Comprehensive Molecular Analytics, Helmholtz Zentrum München, 81379 München, Germany
| | - Jianqiang Zeng
- State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environment Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Hua Fang
- State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environment Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Shaoxuan Xiao
- State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environment Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Michal Pardo
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - Elena Hartner
- Joint Mass Spectrometry Centre, Chair of Analytical Chemistry, Institute of Chemistry, University of Rostock, 18059 Rostock, Germany; Joint Mass Spectrometry Centre, Comprehensive Molecular Analytics, Helmholtz Zentrum München, 81379 München, Germany
| | - Daphne Meidan
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel
| | - Xinming Wang
- State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environment Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
| | - Ralf Zimmermann
- Joint Mass Spectrometry Centre, Chair of Analytical Chemistry, Institute of Chemistry, University of Rostock, 18059 Rostock, Germany; Joint Mass Spectrometry Centre, Comprehensive Molecular Analytics, Helmholtz Zentrum München, 81379 München, Germany
| | - Alexander Laskin
- Department of Chemistry, Purdue University, West Lafayette, IN 47907, USA; Department of Earth, Atmospheric and Planetary Sciences, Purdue University, West Lafayette, IN 47907, USA
| | - Yinon Rudich
- Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel.
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Widespread phytoplankton blooms triggered by 2019-2020 Australian wildfires. Nature 2021; 597:370-375. [PMID: 34526706 DOI: 10.1038/s41586-021-03805-8] [Citation(s) in RCA: 49] [Impact Index Per Article: 16.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/25/2020] [Accepted: 07/05/2021] [Indexed: 11/09/2022]
Abstract
Droughts and climate-change-driven warming are leading to more frequent and intense wildfires1-3, arguably contributing to the severe 2019-2020 Australian wildfires4. The environmental and ecological impacts of the fires include loss of habitats and the emission of substantial amounts of atmospheric aerosols5-7. Aerosol emissions from wildfires can lead to the atmospheric transport of macronutrients and bio-essential trace metals such as nitrogen and iron, respectively8-10. It has been suggested that the oceanic deposition of wildfire aerosols can relieve nutrient limitations and, consequently, enhance marine productivity11,12, but direct observations are lacking. Here we use satellite and autonomous biogeochemical Argo float data to evaluate the effect of 2019-2020 Australian wildfire aerosol deposition on phytoplankton productivity. We find anomalously widespread phytoplankton blooms from December 2019 to March 2020 in the Southern Ocean downwind of Australia. Aerosol samples originating from the Australian wildfires contained a high iron content and atmospheric trajectories show that these aerosols were likely to be transported to the bloom regions, suggesting that the blooms resulted from the fertilization of the iron-limited waters of the Southern Ocean. Climate models project more frequent and severe wildfires in many regions1-3. A greater appreciation of the links between wildfires, pyrogenic aerosols13, nutrient cycling and marine photosynthesis could improve our understanding of the contemporary and glacial-interglacial cycling of atmospheric CO2 and the global climate system.
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