Quantification of carbon dioxide and methane emissions in urban areas: source apportionment based on atmospheric observations

Anthropogenic emissions of carbon dioxide (CO 2 ) and methane (CH 4 ) in the atmosphere constitute an important component of the related carbon budget. The main source of anthropogenic CO 2 is burning of fossil fuels, especially in densely populated areas. Similar emissions of CH 4 are associated wi...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Mitigation and adaptation strategies for global change 2019-08, Vol.24 (6), p.1051-1071
Hauptverfasser: Zimnoch, Miroslaw, Necki, Jaroslaw, Chmura, Lukasz, Jasek, Alina, Jelen, Dorota, Galkowski, Michal, Kuc, Tadeusz, Gorczyca, Zbigniew, Bartyzel, Jakub, Rozanski, Kazimierz
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Anthropogenic emissions of carbon dioxide (CO 2 ) and methane (CH 4 ) in the atmosphere constitute an important component of the related carbon budget. The main source of anthropogenic CO 2 is burning of fossil fuels, especially in densely populated areas. Similar emissions of CH 4 are associated with the agricultural sector, coal mining, and other human activities, such as waste management and storage and natural gas networks supplying methane to large urban, industrial centers. We discuss several methods aimed at characterizing and quantifying atmospheric loads and fluxes of CO 2 and CH 4 in Krakow, the second largest city in Poland. The methods are based on atmospheric observations of mixing ratios as well as isotopic composition of the investigated gases. Atmospheric mixing ratios of CO 2 and CH 4 were measured using gas chromatography (GC) and cavity ring-down spectroscopy (CRDS). The isotopic composition of CO 2 and CH 4 was analyzed using isotope ratio mass spectrometry (IRMS), accelerator mass spectrometry (AMS), and CRDS techniques. These data, combined with auxiliary information characterizing the intensity of vertical mixing in the lower atmosphere (height of the nocturnal boundary layer [NBL] and atmospheric 222 Rn concentration), were further used to quantify emission rates of CO 2 and CH 4 in the urban atmosphere of Krakow. These methods provide an efficient way of quantifying surface emissions of major greenhouse gases originating from distributed sources, thus complementing the widely used bottom-up methodology based on emission statistics.
ISSN:1381-2386
1573-1596
DOI:10.1007/s11027-018-9821-0