Editing IPCC:AR6/WGI/Chapter-6 (section)

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<div id="footnote-004" class="_idFootnote"></div>

[[#footnote-004-backlink|1]] The word ‘concentration’ is used to denote abundances in terms of mixing ratio for most species unless specified.

<div id="footnote-003" class="_idFootnote"></div>

[[#footnote-003-backlink|2]] [[#Prather--2012|Prather et al. (2012)]] report lifetime due to stratospheric loss and soil uptake as 120 ± 24 years and 150 ± 50 years, respectively, and they were inadvertently swapped in AR5 with no effect on the total methane lifetime.

<div id="footnote-002" class="_idFootnote"></div>

[[#footnote-002-backlink|3]] The terms EC and BC are operationally defined on the basis of the methodology used for their quantification (i.e., thermal refractivity and light absorption, respectively) and often used interchangeably.

<div id="footnote-001" class="_idFootnote"></div>

[[#footnote-001-backlink|4]] The carbon mass fraction of OA is termed as OC, a conversion factor between 1.4 to 1.6 from OC to OA is typically assumed.

<div id="footnote-000" class="_idFootnote"></div>

[[#footnote-000-backlink|5]] Baseline ozone is defined as the observed ozone at a site when it is not influenced by recent, locally emitted or anthropogenically produced pollution (Jaffe et al., 2018).

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