Abstract

Abstract. 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.

Highlights

  • Perfluorocarbons (PFCs) are very potent greenhouse gases

  • We present measurements of CF4, C2F6 and C3F8 in air extracted from four firn sites (DSSW20K, EDML, NEEM 2008 and South Pole 2001) and two ice cores (DE08 and DE08-2)

  • The model–data mismatch is lowest for the CF4 background level of 34.05 ppt

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Summary

Introduction

Perfluorocarbons (PFCs) are very potent greenhouse gases (about 7000–11 000 times more powerful than CO2 on a weight-emitted basis over a 100-year timescale; Myhre et al, 2013). CF4 (carbon tetrafluoride, PFC-14) is the most abundant perfluorocarbon in the atmosphere (Mühle et al, 2010) It is released predominantly from aluminium production (due to so-called “anode effects”, when the feed of aluminum oxide to or within the electrolysis cell is restricted; Holiday and Henry, 1959; Tabereaux, 1994) and during semiconductor manufacture (Tsai et al, 2002; Khalil et al, 2003). Other very small industrial sources of CF4 include release during production of SF6 and HCFC-22 (Institute for Environmental Protection and Research, 2013) and from UV photolysis of trifluoroacetyl fluoride, which is a degradation product of halocarbons such as HFC-134a, HCFC-124 and CFC-114a (Jubb et al, 2015) Another possible source of CF4 is from the rare earth industry, in China, neodymium oxide electrolysis (Vogel and Friedrich, 2015).

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