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Improvement In Climate Forcing From Montreal Protocol Gases James W. Elkins1,2, Geoff S. Dutton1,2, Stephen A. Montzka1, James H. Butler1, Debra J. Mondeel1,2, Bradley D. Hall1, Alan M. Yoshinaga1, and David W. Fahey1 1NOAA Earth System Research Laboratory (ESRL), 325 Broadway, Boulder, Colorado, 80305 2Cooperative Institute for Research in Environmental Sciences (CIRES), Boulder, Colorado 80309This year of 2007, an important milestone for CO_2 measurements, marks the 30^th anniversary of the beginning of nitrous oxide (N_2 O) and chlorofluorocarbons (CFCs) measurements by NOAA ESRL scientists at the Mauna Loa Observatory. The 1987 Montreal Protocol on Substances that Deplete the Ozone Layer, which effectively controls emissions of the CFCs, halons, halocarbon solvents, hydro-CFCs or HCFCs, and methyl bromide, was a landmark international agreement that not only controlled the emissions of halocarbons that contributed to the Antarctic Ozone Hole, but had the additional benefit of reducing the emissions of potent greenhouse gases. The CO_2 equivalent reduction in emissions of the Montreal Protocol gases is ~ 8 Gt CO_2 -eq yr^-1 (2.2 Gt C-eq yr^-1 ) between 1990 and 2010. This is four times larger than the reduction in greenhouse gas emissions targeted in the first commitment period of the Kyoto Protocol, which includes CO_2 , CH_4 , N_2 O, SF_6 , hydrofluorocarbons or HFCs, and perfluorocarbons or PFCs.. Over the past couple of years, the atmospheric concentrations of two key halocarbon gases (CFC-12 and halon-1211) have leveled off in the atmosphere. It is important to continue to monitor non-CO_2 greenhouse gases (includes Montreal Protocol Gases, HFCs, CH_4 , N_2 O, and PFCs) in the future, because reducing emissions of these gases may prove to be less difficult in the short term than reducing CO_2 emissions, which will involve major changes in our energy use and the economy. |