“…BC can contribute to temperature change through several mechanisms; absorption of direct and reflected solar radiation Jacobson, 2002;Myhre et al, 2009;Schulz et al, 2006;Skeie et al, 2011), impacts on cloud cover and formation (Ackerman et al, 2000;Cook and Highwood, 2004;Johnson et al, 2004;Koch et al, 2011;Koren et al, 2004;Liu et al, 2009;Penner et al, 2009) and reduction of the surface albedo when deposited on snow and ice (Clarke and Noone, 1985;Flanner et al, 2009;Flanner et al, 2007;Hansen and Nazarenko, 2003;Jacobson, 2004;Rypdal et al, 2009b;Warren and Wiscombe, 1980) The short atmospheric lifetime of BC means that emission reductions will have a rapid response and reduction of BC emissions may be an efficient way of slowing down global warming, especially at high latitudes Bond and Sun, 2005;Hansen et al, 2000;Jacobson, 2002;Kopp and Mauzerall, 2010;Quinn et al, 2008). Such reductions would also have significant co-benefits for air pollution and health (Aunan et al, 2006;Jacobson, 2010;Rypdal et al, 2009a). The implementation of an efficient policy aimed at BC, which is currently not regulated under any global agreements, requires knowledge of where measures are economically and politically most feasible and where the effect on climate is most beneficial (Rypdal et al, 2009b).…”