“…Such the behavior agrees well with other known observations of surface air composition in northern Eurasia, particularly with the data obtained during TROICA (TRanscontinental Observations Into the Chemistry of the Atmosphere) campaigns being conducted regularly since 1996 on the basis of a mobile carriage observatory along the Trans‐Siberian railroad from Moscow–Vladivostok–Moscow [ Elansky , 2009]. According to the TROICA measurements [ Bergamaschi et al , 1998; Belikov et al , 2006; Turnbull et al , 2009], surface CO concentrations over continental northern Eurasia are much higher in winter, which can be explained mainly by the higher static stability of the lower troposphere, lower OH radical concentrations [ Jaffe et al , 1998; Novelli et al , 1998], and higher anthropogenic emissions from heating [ Holloway et al , 2000]. On the basis of the TROICA measurements, the regions of southern Ural and western Siberia (SWS at Figure 1) were earlier identified as the regions with strong biogenic and anthropogenic emissions of many reactive gases, including nitrogen oxides, methane and carbon monoxide [ Bergamaschi et al , 1998; Hurst et al , 2004; Elansky , 2007].…”