Abstract
Abstract. Sulfur hexafluoride (SF6) has a global warming potential of around 22 800 over a 100-year time horizon and is one of the greenhouse gases regulated under the Kyoto Protocol. Around the year 2000 there was a reversal in the global SF6 emission trend, from a decreasing to an increasing trend, which was likely caused by increasing emissions in countries that are not obligated to report their annual emissions to the United Nations Framework Convention on Climate Change. In this study, SF6 emissions during the period 2006–2012 for all East Asian countries – including Mongolia, China, Taiwan, North Korea, South Korea and Japan – were determined by using inverse modeling and in situ atmospheric measurements. We found that the most important sources of uncertainty associated with these inversions are related to the choice of a priori emissions and their assumed uncertainty, the station network as well as the meteorological input data. Much lower uncertainties are due to seasonal variability in the emissions, inversion geometry and resolution, and the measurement calibration scale. Based on the results of these sensitivity tests, we estimate that the total SF6 emission in East Asia increased rapidly from 2404 ± 325 Mg yr−1 in 2006 to 3787 ± 512 Mg yr−1 in 2009 and stabilized thereafter. China contributed 60–72% to the total East Asian emission for the different years, followed by South Korea (8–16%), Japan (5–16%) and Taiwan (4–7%), while the contributions from North Korea and Mongolia together were less than 3% of the total. The per capita SF6 emissions are highest in South Korea and Taiwan, while the per capita emissions for China, North Korea and Japan are close to global average. During the period 2006–2012, emissions from China and from South Korea increased, while emissions from Taiwan and Japan decreased overall.
Highlights
Sulfur hexafluoride (SF6) is one of the greenhouse gases (GHG) regulated under the Kyoto Protocol (UN, 1998)
We evaluated the influence of different a priori emission data sets on the inversion: (1) the reference data set, United Nations Framework Convention on Climate Change (UNFCCC) and East Asian country emissions were disaggregated using the Center for International Earth Science Information Network (CIESIN, 2005) population map (UNFCCC/East Asia/CIESIN, from here on “UC_adjust”); (2) the same as UC_adjust but without East Asian country-specific information (UNFCCC/CIESIN, from here on “UC”); and (3) the gridded SF6 inventory from EDGAR v4.2
Note that the emissions allocation in EDGAR is quite different from the CIESIN (2005) global population map, because EDGAR uses the urban settlements of CIESIN (2005) for an urban population map that was used as a proxy for spatial emission distribution (Janssens-Maenhout et al, 2013)
Summary
Sulfur hexafluoride (SF6) is one of the greenhouse gases (GHG) regulated under the Kyoto Protocol (UN, 1998). Its atmospheric lifetime is estimated to be ∼ 3200 years (Ravishankara et al, 1993). It is the most potent GHG, with a global warming potential (GWP) of 22800 over a 100-year time horizon (Forster et al, 2007). The major source for SF6 to the atmosphere is fugitive emissions from high-voltage electric equipment, while the minor sources are magnesium production, electronics manufacturing, SF6 production and other sources (Olivier et al, 2005). Long-term atmospheric measurements show that the growth rate of the atmospheric SF6 mole fraction has increased again since around the year. X. Fang et al.: Sulfur hexafluoride (SF6) emissions in East Asia
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