“…Uplifted CO usually has a longer lifetime and can be transported fast by the upper layer winds over long distances through continents and between hemispheres in the troposphere (Stohl, 2001;Stohl et al, 2002;Damoah et al, 2004). Uplifting air mass from the surface to FT generally takes place by three processes: (1) frontal lifting, (2) orographic lifting, and (3) deep convection (Brown et al, 1984;Banic et al, 1986;Dickerson et al, 1987;Bethan et al, 1998;Pickering et al, 1998;Chung et al, 1999;Donnell et al, 2001;Kowol-Santen et al, 2001;Cooper et al, 2002;Liu et al, 2003;Miyazaki et al, 2003;Chan et al;Mari et al, 2004;Liu et al, 2006;Kar et al, 2008;Zhao et al, 2008;Ding et al, 2009;Randel et al, 2010;Chen et al, 2012).…”