“…The second factor in the likelihood that variable dry deposition fluxes in different regions may also have influences on CR values, even if the regions share similar precipitation amounts and wet deposition fluxes. For example, due to different dry deposition fluxes (430, 220, and 38 mg m À2 yr À1 for Jersey City, New Brunswick, and Tuckerton, respectively), higher CR PAHs value occurred in Tuckerton (0.69), but lower values appeared in Jersey City (0.27) and New Brunswick (0.26), although these three areas had similar wet deposition fluxes (76, 160 and 84 mg m À2 yr À1 ) for Jersey City, New Brunswick and Tuckerton (Gigliotti et al, 2005). Golomb et al (2001) showed that different dry deposition fluxes of PAHs among different regions were mainly associated with different types of source inputs and emission amounts, e.g., the much higher F dry value in Nahant than that in Wolfs Neck (Table S9) was likely due to higher emissions of PAHs from civil aircraft and automobile exhausts (Golomb et al, 2001).…”