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  3. Atmospheric abundance and global emissions of perfluorocarbons CF₄, C2F₆ and C₃F₈ since 1800 inferred from ice core, firn, air archive and in situ measurements
 

Atmospheric abundance and global emissions of perfluorocarbons CF₄, C2F₆ and C₃F₈ since 1800 inferred from ice core, firn, air archive and in situ measurements

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BORIS DOI
10.7892/boris.93426
Publisher DOI
10.5194/acp-16-11733-2016
Description
Perfluorocarbons (PFCs) are very potent and long-lived greenhouse gases in the atmosphere, released predominantly during aluminium production and semiconductor manufacture. They have been targeted for emission controls under the United Nations Framework Convention on Climate Change. Here we present the first continuous records of the atmospheric abundance of CF4 (PFC-14), C₂F₆ (PFC-116) and C₃F₈ (PFC-218) from 1800 to 2014. The records are derived from high-precision measurements of PFCs in air extracted from polar firn or ice at six sites (DE08, DE08-2, DSSW20K, EDML, NEEM and South Pole) and air archive tanks and atmospheric air sampled from both hemispheres. We take account of the age characteristics of the firn and ice core air samples and demonstrate excellent consistency between the ice core, firn and atmospheric measurements. We present an inversion for global emissions from 1900 to 2014. We also formulate the inversion to directly infer emission factors for PFC emissions due to aluminium production prior to the 1980s. We show that 19th century atmospheric levels, before significant anthropogenic influence, were stable at 34.1 ± 0.3 ppt for CF₄ and below detection limits of 0.002 and 0.01 ppt for C₂F₆ and C₃F₈, respectively. We find a significant peak in CF₄ and C₂F₆ emissions around 1940, most likely due to the high demand for aluminium during World War II, for example for construction of aircraft, but these emissions were nevertheless much lower than in recent years. The PFC emission factors for aluminium production in the early 20th century were significantly higher than today but have decreased since then due to improvements and better control of the smelting process. Mitigation efforts have led to decreases in emissions from peaks in 1980 (CF₄) or early-to-mid-2000s (C₂F₆ and C₃F₈) despite the continued increase in global aluminium production; however, these decreases in emissions appear to have recently halted. We see a temporary reduction of around 15 % in CF₄ emissions in 2009, presumably associated with the impact of the global financial crisis on aluminium and semiconductor production.
Date of Publication
2016
Publication Type
Article
Subject(s)
500 Science > 530 Physics
Language(s)
en
Contributor(s)
Trudinger, Cathy M.
Fraser, Paul J.
Etheridge, David M.
Sturges, William T.
Vollmer, Martin K.
Rigby, Matt
Martinerie, Patricia
Mühle, Jens
Worton, David R.
Krummel, Paul B.
Steele, L. Paul
Miller, Benjamin R.
Laube, Johannes
Mani, Francis S.
Rayner, Peter J.
Harth, Christina M.
Witrant, Emmanuel
Blunier, Thomas
Schwander, Jakob
Physikalisches Institut, Klima- und Umweltphysik (KUP)
O'Doherty, Simon
Battle, Mark
Additional Credits
Physikalisches Institut, Klima- und Umweltphysik (KUP)
Series
Atmospheric chemistry and physics
Publisher
European Geosciences Union
ISSN
1680-7316
Access(Rights)
open.access
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