“…It remains difficult to quantify the contribution of precursors in the ambient environment. Several field‐based methods have been developed to estimate the amount of SOA, including the tracer‐yield method (Guo et al, 2012; Kleindienst et al, 2007), the nonprimary organic carbon (OC) method (the receptor model) (Heo et al, 2015; Yuan et al, 2006; Zheng et al, 2002), the non–biomass burning water‐soluble organic carbon method (Weber et al, 2007) and the elemental carbon (EC)‐tracer method (or the OC/EC ratio method) [Cao et al, 2007; Song Guo et al, 2014; Turpin & Huntzicker, 1995; Zhang et al, 2008]. Among these methods, the receptor model can be used to apportion SOA in submicron particulate matter (PM 1.0 ) at a high time resolution from aerosol mass spectrometry (AMS) data (Hu et al, 2013; Huang et al, 2012; Huang et al, 2014; Li et al, 2015; Sun et al, 2013; Zhang, 2005), while the tracer‐yield method provides the only way of identifying precursors of SOA but with a low time resolution due to the complexity of tracer measurements.…”