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==== 6.3.3.5 Sulphur Dioxide (SO <sub>2</sub> ) ==== <div id="h3-13-siblings" class="h3-siblings"></div> The AR5 did not assess trends in SO <sub>2</sub> concentrations. Trends in SO <sub>2</sub> abundances are consistent with the overall anthropogenic emissions changes as presented in Section 6.2 and Figure 6.18. Long-term surface-based in situ observations in North America and Europe show reductions of more than 80% since the measurements began around 1980 (Table 6.5). Europe had the largest reductions in the first part of the period while the highest reduction came later in North America. Observed trends are qualitatively reproduced by global and regional models over North America and Europe during the period 1990β2015 for which emissions changes are well quantified (Table 6.5; [[#Aas--2019|Aas et al., 2019]] ). <div id="_idContainer023" class="_idGenObjectStyleOverride-1"></div> '''Table 6.5 |''' '''Summary of changes or trends in atmospheric abundance of sulphur dioxide (SO''' <sub>2</sub> ''') and sulphate (SO''' <sub>4</sub> <sup>2β</sup> ''') aerosols based on in situ and satellite observations.''' {| class="wikitable" |- | '''Analysis Period''' | '''Trends in SO''' <sub>2</sub> | '''Trends in Particulate SO''' <sub>4</sub> <sup>2β</sup> | '''Reference''' |- | colspan="4"| Global Models/Assimilated Models |- | 1990β2000 | β8.54 Β± 1.40% yr <sup>β1</sup> (EU, 43 sites) β2.63 Β± 0.30% yr <sup>β1</sup> (NA, 53 sites) | β5.23 Β± 1.17% yr <sup>β1</sup> (EU, 41 sites) β1.94 Β± 0.43% yr <sup>β</sup> (NA 101 sites) | [[#Aas--2019|Aas et al. (2019)]] |- | 2000β2015 | β0.41 Β± 0.92% yr <sup>β1</sup> (EA, 19 sites) β4.86 Β± 1.31% yr <sup>β1</sup> (EU, 47 sites) β4.40 Β± 0.93% yr <sup>β1</sup> (NA, 77 sites) | 0.02 Β± 0.91% yr <sup>β1</sup> (EA, 13 sites) β3.26 Β± 0.85% yr <sup>β1</sup> (EU, 36 sites) β3.18 Β± 0.66% yr <sup>β1</sup> (NA, 218 sites) | [[#Aas--2019|Aas et al. (2019)]] |- | colspan="4"| Ground-based In Situ Observations |- | 1980β1990 | β5.03 Β± 2.04% yr <sup>β1</sup> (EU, 20 sites) β2.5% yr <sup>β1</sup> (US) | β2.56 Β± 3.10% yr <sup>β1</sup> (EU, 16 sites) β1.80 Β± 4.09% yr <sup>β1</sup> (US SO <sub>4</sub> <sup>2β</sup> in precipitation, 78 sites) | [[#Aas--2019|Aas et al. (2019)]] [https://www.epa.gov/air-trends/sulfur-dioxide-trends US EPA] <sup>a</sup> |- | 1990β2000 | β7.56 Β± 1.81% yr <sup>β1</sup> (EU, 43 sites) β3.27 Β± 1.69% yr <sup>β1</sup> (NA, 53 sites) | β5.16 Β± 2.11% yr <sup>β1</sup> (EU, 41 sites) β2.08 Β± 1.44% yr <sup>β1</sup> (NA, 101 sites) | [[#Aas--2019|Aas et al. (2019)]] |- | 2000β2015 | β0.14 Β± 5.32% yr <sup>β1</sup> (EA, 19 sites) β3.89 Β± 2.16% yr <sup>β1</sup> (EU, 47 sites) β4.69 Β± 1.35% yr <sup>β1</sup> (NA, 77 sites) | 2.68 Β± 9.41% yr <sup>β1</sup> (EA, 13 sites) β2.67 Β± 2.03% yr <sup>β1</sup> (EU, 36 sites) β3.15 Β± 1.30% yr <sup>β1</sup> (NA, 218 sites) | [[#Aas--2019|Aas et al. (2019)]] |- | colspan="4"| Change Based on Satellite Observations |- | 2005β2015 | ca β80% (Eastern US) | | [[#Krotkov--2016|Krotkov et al. (2016)]] |- | 2005β2015 | ca β60% (Eastern EU) | | [[#Krotkov--2016|Krotkov et al. (2016)]] |- | 2005β2015 | 200 Β± 50% (India) | | [[#Krotkov--2016|Krotkov et al. (2016)]] |- | 2005 (and 2012) β2015 | ca β50% (The North China Plain) | | [[#Krotkov--2016|Krotkov et al. (2016)]] |} <sup>a</sup> https://www.epa.gov/air-trends/sulfur-dioxide-trends In situ observations over other parts of the world are scattered. However, the limited in situ observations in Eastern Asia indicate an increase in atmospheric SO <sub>2</sub> up to around 2005 and then a decline ( [[#Aas--2019|Aas et al., 2019]] ). This is confirmed by satellite observations ( [[#Krotkov--2016|Krotkov et al., 2016]] ), which further reveal a rapid decline in SO <sub>2</sub> since around 2012 or 2013 ( [[#Krotkov--2016|Krotkov et al., 2016]] ; [[#Zheng--2018b|Zheng et al., 2018b]] ). In India, on the other hand, SO <sub>2</sub> levels have doubled between 2005 and 2015 ( [[#Krotkov--2016|Krotkov et al., 2016]] ). In summary, surface and satellite observations indicate strong regional variations in trends of atmospheric SO <sub>2</sub> abundance. The SO <sub>2</sub> concentrations in North America and Europe have declined over 1980β2015 with slightly stronger reductions in North America (70 Β± 20%) than in Europe (58 Β± 32%) over 2000β2015, though Europe had larger reductions than the US in the prior decade (1990β2000). In Asia, the SO <sub>2</sub> trends are more scattered, though there is ''medium confidence'' that there was a strong increase up to around 2005, followed by a steep decline in China, while over India, the concentrations are increasing steadily. <div id="6.3.4" class="h2-container"></div> <span id="short-lived-halogenated-species"></span>
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