“…Many qualitative outcomes of forcing by anthropogenic GHGs have been postulated, such as changes in standard ocean-atmosphere variables of wind, water vapor, rain, snow, land and sea ice, sea level, and the frequency and intensity of extreme events such as storms and hurricanes (Soon et al 1999), as well as more exotic phenomena, including large cooling of the mesosphere and thermosphere (Akmaev & Fomichev 2000), increased presence or brightness of noctilucent clouds near the polar summer mesopause (Thomas 1996, but see Gadsden 1998), increases in atmospheric angular momentum and length of day (Abarca del Rio 1999, Huang et al 2001), and shrinking of surfaces of constant density at operating satellite altitudes (Keating et al 2000). In these calculations, the benchmark forcing scenario is usually an emission rate of 1% yr -1 chosen to represent roughly the CO 2 equivalent of the burden of all anthropogenic GHGs.…”