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Fratticioli C, Trisolino P, Maione M, Calzolari F, Calidonna C, Biron D, Amendola S, Steinbacher M, Cristofanelli P. Continuous atmospheric in-situ measurements of the CH 4/CO ratio at the Mt. Cimone station (Italy, 2165 m a.s.l.) and their possible use for estimating regional CH 4 emissions. Environ Res 2023:116343. [PMID: 37321340 DOI: 10.1016/j.envres.2023.116343] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/28/2023] [Revised: 05/21/2023] [Accepted: 06/05/2023] [Indexed: 06/17/2023]
Abstract
Methane (CH4) is an important climate forcer, contributing about 17% of the total radiative forcing by long living greenhouse gases. The Po basin is one of the most polluted and densely populated areas in Europe representing an important source region for CH4. The aim of this work was to test an inter-species correlation approach to derive estimates of anthropogenic CH4 emissions for the period 2015-2019 from the Po basin by combining CO bottom-up inventory data and continuous CH4 and CO observations from a mountain site in the northern Italy. The tested methodology suggested lower emissions in respect to EDGAR (-17%) and the Italian National Inventory (-40%) for the Po basin. However, despite the two bottom-up inventories, the emissions derived from the atmospheric observations reported an increasing tendency from 2015 to 2019 for the CH4 emissions. A sensitivity study revealed that using different subsets of the atmospheric observations implied a difference of 26% in the CH4 emission estimates. The highest agreement with two bottom-up CH4 inventories (EDGAR and the Italian national inventory) were obtained when atmospheric data were strictly selected for periods representative of air mass transport from the Po basin. Our study identified various challenges when using this methodology as a benchmark to verify bottom-up CH4 inventories. Issues could be attributed to the annual aggregation of the proxies used to derive the emission amounts, to the CO bottom-up inventory used as input information and to the relatively high sensitivity of the results to the different subsets of the atmospheric observations. However, the use of different bottom-up inventories as input data for CO emissions can potentially provide information that should be carefully considered for the purpose of integrating CH4 bottom-up inventories.
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Affiliation(s)
| | - P Trisolino
- CNR-ISAC, Via Gobetti 101, 40129, Bologna, Italy
| | - M Maione
- University of Urbino - Faculty of Science and Technologies, Piazza Rinascimento 6, Urbino, 61029, Italy
| | - F Calzolari
- CNR-ISAC, Via Gobetti 101, 40129, Bologna, Italy
| | - C Calidonna
- CNR-ISAC, Zona Industriale-Comparto 15-presso Fondazione Mediterranea Terina, I-88046, Lamezia Terme, CZ, Italy
| | - D Biron
- Aeronautica Militare, CAMM - Monte Cimone, Via delle Ville, 40 - 41029 Sestola, MO, Italy
| | - S Amendola
- Aeronautica Militare, CAMM - Monte Cimone, Via delle Ville, 40 - 41029 Sestola, MO, Italy
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Ramonet M, Ciais P, Apadula F, Bartyzel J, Bastos A, Bergamaschi P, Blanc PE, Brunner D, Caracciolo di Torchiarolo L, Calzolari F, Chen H, Chmura L, Colomb A, Conil S, Cristofanelli P, Cuevas E, Curcoll R, Delmotte M, di Sarra A, Emmenegger L, Forster G, Frumau A, Gerbig C, Gheusi F, Hammer S, Haszpra L, Hatakka J, Hazan L, Heliasz M, Henne S, Hensen A, Hermansen O, Keronen P, Kivi R, Komínková K, Kubistin D, Laurent O, Laurila T, Lavric JV, Lehner I, Lehtinen KEJ, Leskinen A, Leuenberger M, Levin I, Lindauer M, Lopez M, Myhre CL, Mammarella I, Manca G, Manning A, Marek MV, Marklund P, Martin D, Meinhardt F, Mihalopoulos N, Mölder M, Morgui JA, Necki J, O'Doherty S, O'Dowd C, Ottosson M, Philippon C, Piacentino S, Pichon JM, Plass-Duelmer C, Resovsky A, Rivier L, Rodó X, Sha MK, Scheeren HA, Sferlazzo D, Spain TG, Stanley KM, Steinbacher M, Trisolino P, Vermeulen A, Vítková G, Weyrauch D, Xueref-Remy I, Yala K, Yver Kwok C. The fingerprint of the summer 2018 drought in Europe on ground-based atmospheric CO 2 measurements. Philos Trans R Soc Lond B Biol Sci 2020; 375:20190513. [PMID: 32892733 DOI: 10.1098/rstb.2019.0513] [Citation(s) in RCA: 17] [Impact Index Per Article: 4.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/12/2022] Open
Abstract
During the summer of 2018, a widespread drought developed over Northern and Central Europe. The increase in temperature and the reduction of soil moisture have influenced carbon dioxide (CO2) exchange between the atmosphere and terrestrial ecosystems in various ways, such as a reduction of photosynthesis, changes in ecosystem respiration, or allowing more frequent fires. In this study, we characterize the resulting perturbation of the atmospheric CO2 seasonal cycles. 2018 has a good coverage of European regions affected by drought, allowing the investigation of how ecosystem flux anomalies impacted spatial CO2 gradients between stations. This density of stations is unprecedented compared to previous drought events in 2003 and 2015, particularly thanks to the deployment of the Integrated Carbon Observation System (ICOS) network of atmospheric greenhouse gas monitoring stations in recent years. Seasonal CO2 cycles from 48 European stations were available for 2017 and 2018. Earlier data were retrieved for comparison from international databases or national networks. Here, we show that the usual summer minimum in CO2 due to the surface carbon uptake was reduced by 1.4 ppm in 2018 for the 10 stations located in the area most affected by the temperature anomaly, mostly in Northern Europe. Notwithstanding, the CO2 transition phases before and after July were slower in 2018 compared to 2017, suggesting an extension of the growing season, with either continued CO2 uptake by photosynthesis and/or a reduction in respiration driven by the depletion of substrate for respiration inherited from the previous months due to the drought. For stations with sufficiently long time series, the CO2 anomaly observed in 2018 was compared to previous European droughts in 2003 and 2015. Considering the areas most affected by the temperature anomalies, we found a higher CO2 anomaly in 2003 (+3 ppm averaged over 4 sites), and a smaller anomaly in 2015 (+1 ppm averaged over 11 sites) compared to 2018. This article is part of the theme issue 'Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale'.
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Affiliation(s)
- M Ramonet
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - P Ciais
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - F Apadula
- Ricerca sul Sistema Energetico, Milan, Italy
| | - J Bartyzel
- AGH University of Science and Technology, 30059 Krakow, Poland
| | - A Bastos
- Department of Geography, Ludwig-Maximilians University, 80333 Munich, Germany
| | - P Bergamaschi
- European Commission, Joint Research Centre, Ispra, Italy
| | - P E Blanc
- Aix Marseille Univ, Avignon Université, CNRS, IRD, Institut Méditerranéen de Biodiversité et d'Ecologie marine et continentale (IMBE), Marseille, France
| | - D Brunner
- Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, Switzerland
| | | | - F Calzolari
- National Research Council, Institute of Atmospheric Sciences and Climate, Bologna, Italy
| | - H Chen
- Centre for Isotope Research (CIO), University of Groningen, Nijenborgh 6, 9747 AG Groningen, The Netherlands
| | - L Chmura
- AGH University of Science and Technology, 30059 Krakow, Poland
| | - A Colomb
- Université Clermont Auvergne, CNRS, Laboratoire de Météorologie Physique, UMR 6016, Clermont-Ferrand, France
| | - S Conil
- DRD/OPE, Andra, Bure, France
| | - P Cristofanelli
- National Research Council, Institute of Atmospheric Sciences and Climate, Bologna, Italy
| | - E Cuevas
- Izana Atmospheric Research Center, Meteorological State Agency of Spain, Tenerife, Spain
| | - R Curcoll
- Institut de Ciencia i Tecnologia Ambientals, Universitat Autonoma de Barcelona, Barcelona, Spain
| | - M Delmotte
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - A di Sarra
- Agenzia Nazionale per le Nuove Tecnologie, l'Energia e lo Sviluppo Economico Sostenibile, Rome, Italy
| | - L Emmenegger
- Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, Switzerland
| | - G Forster
- National Centre for Atmospheric Science, University of East Anglia, Norwich, UK
| | - A Frumau
- Netherlands Organisation for Applied Scientific Research, Petten, The Netherlands
| | - C Gerbig
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - F Gheusi
- Laboratoire d'Aérologie, UPS Université Toulouse 3, CNRS (UMR5560), Toulouse, France
| | - S Hammer
- University of Heidelberg, Institut fuer Umweltphysik, Heidelberg, Germany
| | - L Haszpra
- Research Centre for Astronomy and Earth Sciences, Sopron, Hungary
| | - J Hatakka
- Finnish Meteorological Institute, Helsinki, Finland
| | - L Hazan
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - M Heliasz
- Centre for Environmental and Climate Research, Lund University, Lund, Sweden
| | - S Henne
- Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, Switzerland
| | - A Hensen
- Netherlands Organisation for Applied Scientific Research, Petten, The Netherlands
| | - O Hermansen
- NILU - Norwegian Institute for Air Research, Oslo, Norway
| | - P Keronen
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - R Kivi
- Finnish Meteorological Institute, Helsinki, Finland
| | - K Komínková
- Global Change Research Institute of the Czech Academy of Sciences, Brno, Czech Republic
| | - D Kubistin
- Deutscher Wetterdienst, Hohenpeißenberg Meteorological Observatory, Hohenpeißenberg, Germany
| | - O Laurent
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - T Laurila
- Finnish Meteorological Institute, Helsinki, Finland
| | - J V Lavric
- Max Planck Institute for Biogeochemistry, Jena, Germany
| | - I Lehner
- Centre for Environmental and Climate Research, Lund University, Lund, Sweden
| | - K E J Lehtinen
- Finnish Meteorological Institute, Helsinki, Finland.,University of Eastern Finland, Kuopio, Finland
| | - A Leskinen
- Finnish Meteorological Institute, Helsinki, Finland.,University of Eastern Finland, Kuopio, Finland
| | - M Leuenberger
- University of Bern, Physics Institute, Climate and Environmental Physics Division and Oeschger Center for Climate Change Research, Bern, Switzerland
| | - I Levin
- University of Heidelberg, Institut fuer Umweltphysik, Heidelberg, Germany
| | - M Lindauer
- Deutscher Wetterdienst, Hohenpeißenberg Meteorological Observatory, Hohenpeißenberg, Germany
| | - M Lopez
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - C Lund Myhre
- NILU - Norwegian Institute for Air Research, Oslo, Norway
| | - I Mammarella
- Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, Helsinki, Finland
| | - G Manca
- European Commission, Joint Research Centre, Ispra, Italy
| | - A Manning
- National Centre for Atmospheric Science, University of East Anglia, Norwich, UK
| | - M V Marek
- Global Change Research Institute of the Czech Academy of Sciences, Brno, Czech Republic
| | - P Marklund
- Swedish University of Agricultural Sciences, Unit for Field-based Forest Research, 92291 Vindeln, Sweden
| | - D Martin
- Environmental Protection Agency, Dublin, Ireland
| | | | - N Mihalopoulos
- Environmental Chemical Processes Laboratory, University of Crete, Greece
| | - M Mölder
- Department of Physical Geography and Ecosystem Science (INES), Lund University, Lund, Sweden
| | - J A Morgui
- Institut de Ciencia i Tecnologia Ambientals, Universitat Autonoma de Barcelona, Barcelona, Spain
| | - J Necki
- AGH University of Science and Technology, 30059 Krakow, Poland
| | - S O'Doherty
- Atmospheric Chemistry Research Group School of Chemistry, University of Bristol, Bristol, UK
| | - C O'Dowd
- National University of Ireland Galway, Galway, Ireland
| | - M Ottosson
- Swedish University of Agricultural Sciences, Unit for Field-based Forest Research, 92291 Vindeln, Sweden
| | - C Philippon
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - S Piacentino
- Agenzia Nazionale per le Nuove Tecnologie, l'Energia e lo Sviluppo Economico Sostenibile, Rome, Italy
| | - J M Pichon
- Université Clermont Auvergne, CNRS, Laboratoire de Météorologie Physique, UMR 6016, Clermont-Ferrand, France
| | - C Plass-Duelmer
- Deutscher Wetterdienst, Hohenpeißenberg Meteorological Observatory, Hohenpeißenberg, Germany
| | - A Resovsky
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - L Rivier
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - X Rodó
- Climate and Health Programme (CLIMA), Barcelona Institute for Global Health (ISGLOBAL), Barcelona, Spain.,Institució Catalana de Recerca i Estudis Avancats (ICREA), Barcelona, Spain
| | - M K Sha
- Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium
| | - H A Scheeren
- Centre for Isotope Research (CIO), University of Groningen, Nijenborgh 6, 9747 AG Groningen, The Netherlands
| | - D Sferlazzo
- Agenzia Nazionale per le Nuove Tecnologie, l'Energia e lo Sviluppo Economico Sostenibile, Rome, Italy
| | - T G Spain
- National University of Ireland Galway, Galway, Ireland
| | - K M Stanley
- Atmospheric Chemistry Research Group School of Chemistry, University of Bristol, Bristol, UK.,Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
| | - M Steinbacher
- Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, Switzerland
| | - P Trisolino
- National Research Council, Institute of Atmospheric Sciences and Climate, Bologna, Italy
| | | | - G Vítková
- Global Change Research Institute of the Czech Academy of Sciences, Brno, Czech Republic
| | - D Weyrauch
- Deutscher Wetterdienst, Hohenpeißenberg Meteorological Observatory, Hohenpeißenberg, Germany
| | - I Xueref-Remy
- Aix Marseille Univ, Avignon Université, CNRS, IRD, Institut Méditerranéen de Biodiversité et d'Ecologie marine et continentale (IMBE), Marseille, France
| | - K Yala
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
| | - C Yver Kwok
- Université Paris-Saclay, CEA, CNRS, UVSQ, Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL), Gif-sur-Yvette, France
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Cesari D, De Benedetto GE, Bonasoni P, Busetto M, Dinoi A, Merico E, Chirizzi D, Cristofanelli P, Donateo A, Grasso FM, Marinoni A, Pennetta A, Contini D. Seasonal variability of PM 2.5 and PM 10 composition and sources in an urban background site in Southern Italy. Sci Total Environ 2018; 612:202-213. [PMID: 28850839 DOI: 10.1016/j.scitotenv.2017.08.230] [Citation(s) in RCA: 73] [Impact Index Per Article: 12.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/07/2017] [Revised: 08/21/2017] [Accepted: 08/22/2017] [Indexed: 06/07/2023]
Abstract
Comparison of fine and coarse fractions in terms of sources and dynamics is scarce in southeast Mediterranean countries; differences are relevant because of the importance of natural sources like sea spray and Saharan dust advection, because most of the monitoring networks are limited to PM10. In this work, the main seasonal variabilities of sources and processes involving fine and coarse PM (particulate matter) were studied at the Environmental-Climate Observatory of Lecce (Southern Italy). Simultaneous PM2.5 and PM10 samples were collected between July 2013 and July 2014 and chemically analysed to determine concentrations of several species: OC (organic carbon) and EC (elemental carbon) via thermo-optical analysis, 9 major ions via IC, and 23 metals via ICP-MS. Data was processed through mass closure analysis and Positive Matrix Factorization (PMF) receptor model characterizing seasonal variabilities of nine sources contributions. Organic and inorganic secondary aerosol accounts for 43% of PM2.5 and 12% of PM2.5-10 with small seasonal changes. SIA (secondary inorganic aerosol) seasonal pattern is opposite to that of SOC (secondary organic carbon). SOC is larger during the cold period, sulphate (the major contributor to SIA) is larger during summer. Two forms of nitrate were identified: NaNO3, correlated with chloride depletion and aging of sea-spray, mainly present in PM2.5-10; NH4NO3 more abundant in PM2.5. Biomass burning is a relevant source with larger contribution during autumn and winter because of the influence of domestic heating, however, is not negligible in spring and summer, because of the contributions of fires and agricultural practices. Mass closure analysis and PMF results identify two soil sources: crustal associated to long range transport and carbonates associated to local resuspended dust. Both sources contributes to the coarse fraction and have different dynamics with crustal source contributing mainly in high winds from SE conditions and carbonates during high winds from North direction.
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Affiliation(s)
- D Cesari
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy.
| | - G E De Benedetto
- Dipartimento di Beni Culturali, Università del Salento, 73100 Lecce, Italy
| | - P Bonasoni
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 40129 Bologna, Italy
| | - M Busetto
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 40129 Bologna, Italy
| | - A Dinoi
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy
| | - E Merico
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy
| | - D Chirizzi
- Dipartimento di Beni Culturali, Università del Salento, 73100 Lecce, Italy
| | - P Cristofanelli
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 40129 Bologna, Italy
| | - A Donateo
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy
| | - F M Grasso
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy
| | - A Marinoni
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 40129 Bologna, Italy
| | - A Pennetta
- Dipartimento di Beni Culturali, Università del Salento, 73100 Lecce, Italy
| | - D Contini
- Istituto di Scienze dell'Atmosfera e del Clima, ISAC-CNR, 73100 Lecce, Italy
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