first_pagesettingsOrder Article Reprints Open AccessArticle Expanding Continuous Carbon Isotope Measurements of CO2 and CH4 in the Italian ICOS Atmospheric Consortium: First Results from the Continental POT Station in Potenza (Basilicata) by Antonella Buono 1,*ORCID,Isabella Zaccardo 1,2ORCID,Francesco D’Amico 3,4,*ORCID,Emilio Lapenna 1ORCID,Francesco Cardellicchio 1ORCID,Teresa Laurita 1ORCID,Davide Amodio 1ORCID,Canio Colangelo 1ORCID,Gianluca Di Fiore 1,Aldo Giunta 1ORCID,Michele Volini 1ORCID,Claudia Roberta Calidonna 3ORCID,Alcide Giorgio di Sarra 5ORCID,Serena Trippetta 1ORCID andLucia Mona 1ORCID 1 Institute of Methodologies for Environmental Analysis, National Research Council of Italy (CNR-IMAA), Contrada S. Loja, Tito Scalo, I-85050 Potenza, Italy 2 Department of Engineering, University of Basilicata (Unibas DiING), Via dell’Ateneo Lucano 10, I-85100 Potenza, Italy 3 Institute of Atmospheric Sciences and Climate, National Research Council of Italy (CNR-ISAC), Area Industriale Comparto 15, Lamezia Terme, I-88046 Catanzaro, Italy 4 Department of Biology, Ecology and Earth Sciences, University of Calabria (Unical DiBEST), Via Pietro Bucci Cubo 15B, Rende, I-87036 Cosenza, Italy 5 Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA), Via Enrico Fermi 45, Frascati, I-00044 Rome, Italy * Authors to whom correspondence should be addressed. Atmosphere 2025, 16(8), 951; https://doi.org/10.3390/atmos16080951 Submission received: 30 June 2025 / Revised: 17 July 2025 / Accepted: 6 August 2025 / Published: 8 August 2025 (This article belongs to the Section Air Pollution Control) Downloadkeyboard_arrow_down Browse Figures Versions Notes Abstract Carbon isotope fractionation is an efficient tool used for the discrimination and differentiation of sinks and emission sources. Carbon dioxide (CO2) and methane (CH4) are among the key drivers of climate change, and a detailed evaluation of variations in the 13C/12C ratio in either compound provides vital information for the field of atmospheric sciences. The Italian atmospheric ICOS (Integrated Carbon Observation System) consortium is currently implementing δ13C-CO2 and δ13C-CH4 measurements, with four observation sites now equipped with Picarro G2201-i CRDS (Cavity Ring-Down Spectrometry) analyzers. In this work, results from the first two months of measurements performed at the Potenza station in southern Italy between 20 February and 20 April 2025 are presented and constitute the first evaluation of continuous atmospheric δ13C-CO2 and δ13C-CH4 measurements from an Italian station. These results provide a first insight on how these measurements can improve the current understanding of CO2 and CH4 variability in the Italian peninsula and the central Mediterranean sector. Although preliminary in nature, the findings of these measurements indicate that fossil fuel burning is responsible for the observed peaks in CO2 concentrations. CH4 has a generally stable pattern; however, abrupt peaks in its isotopic delta, observed during March, may constitute the first direct evidence in Italy of Saharan dust intrusion affecting carbon isotope fractionation in the atmosphere. This study also introduces an analysis of the weekly behavior in isotopic deltas.

Expanding Continuous Carbon Isotope Measurements of CO2 and CH4 in the Italian ICOS Atmospheric Consortium: First Results from the Continental POT Station in Potenza (Basilicata)

D'Amico, Francesco
Conceptualization
;
Calidonna, Claudia Roberta
Membro del Collaboration Group
;
2025-01-01

Abstract

first_pagesettingsOrder Article Reprints Open AccessArticle Expanding Continuous Carbon Isotope Measurements of CO2 and CH4 in the Italian ICOS Atmospheric Consortium: First Results from the Continental POT Station in Potenza (Basilicata) by Antonella Buono 1,*ORCID,Isabella Zaccardo 1,2ORCID,Francesco D’Amico 3,4,*ORCID,Emilio Lapenna 1ORCID,Francesco Cardellicchio 1ORCID,Teresa Laurita 1ORCID,Davide Amodio 1ORCID,Canio Colangelo 1ORCID,Gianluca Di Fiore 1,Aldo Giunta 1ORCID,Michele Volini 1ORCID,Claudia Roberta Calidonna 3ORCID,Alcide Giorgio di Sarra 5ORCID,Serena Trippetta 1ORCID andLucia Mona 1ORCID 1 Institute of Methodologies for Environmental Analysis, National Research Council of Italy (CNR-IMAA), Contrada S. Loja, Tito Scalo, I-85050 Potenza, Italy 2 Department of Engineering, University of Basilicata (Unibas DiING), Via dell’Ateneo Lucano 10, I-85100 Potenza, Italy 3 Institute of Atmospheric Sciences and Climate, National Research Council of Italy (CNR-ISAC), Area Industriale Comparto 15, Lamezia Terme, I-88046 Catanzaro, Italy 4 Department of Biology, Ecology and Earth Sciences, University of Calabria (Unical DiBEST), Via Pietro Bucci Cubo 15B, Rende, I-87036 Cosenza, Italy 5 Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA), Via Enrico Fermi 45, Frascati, I-00044 Rome, Italy * Authors to whom correspondence should be addressed. Atmosphere 2025, 16(8), 951; https://doi.org/10.3390/atmos16080951 Submission received: 30 June 2025 / Revised: 17 July 2025 / Accepted: 6 August 2025 / Published: 8 August 2025 (This article belongs to the Section Air Pollution Control) Downloadkeyboard_arrow_down Browse Figures Versions Notes Abstract Carbon isotope fractionation is an efficient tool used for the discrimination and differentiation of sinks and emission sources. Carbon dioxide (CO2) and methane (CH4) are among the key drivers of climate change, and a detailed evaluation of variations in the 13C/12C ratio in either compound provides vital information for the field of atmospheric sciences. The Italian atmospheric ICOS (Integrated Carbon Observation System) consortium is currently implementing δ13C-CO2 and δ13C-CH4 measurements, with four observation sites now equipped with Picarro G2201-i CRDS (Cavity Ring-Down Spectrometry) analyzers. In this work, results from the first two months of measurements performed at the Potenza station in southern Italy between 20 February and 20 April 2025 are presented and constitute the first evaluation of continuous atmospheric δ13C-CO2 and δ13C-CH4 measurements from an Italian station. These results provide a first insight on how these measurements can improve the current understanding of CO2 and CH4 variability in the Italian peninsula and the central Mediterranean sector. Although preliminary in nature, the findings of these measurements indicate that fossil fuel burning is responsible for the observed peaks in CO2 concentrations. CH4 has a generally stable pattern; however, abrupt peaks in its isotopic delta, observed during March, may constitute the first direct evidence in Italy of Saharan dust intrusion affecting carbon isotope fractionation in the atmosphere. This study also introduces an analysis of the weekly behavior in isotopic deltas.
2025
stable carbon isotopes; δ13C; carbon dioxide; methane; Potenza
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.11770/388017
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