Atmospheric Chemistry and Physics, vol. 12, issue 7 (2012) pp. 3333-3348
We calculate decadal aerosol direct and indi- rect (warm cloud) radiative forcings from US anthropogenic sources over the 1950–2050 period. Past and future aerosol distributions are constructed using GEOS-Chem and histor- ical emission inventories and future projections from the IPCC A1B scenario. Aerosol simulations are evaluated with observed spatial distributions and 1980–2010 trends of aerosol concentrations and wet deposition in the contiguous US. Direct and indirect radiative forcing is calculated us- ing the GISS general circulation model and monthly mean aerosol distributions from GEOS-Chem. The radiative forc- ing from US anthropogenic aerosols is strongly localized over the eastern US. We find that its magnitude peaked in 1970–1990, with values over the eastern US (east of 100◦ W) of −2.0Wm−2 for direct forcing including contributions from sulfate (−2.0Wm−2), nitrate (−0.2Wm−2), organic carbon (−0.2Wm−2), and black carbon (+0.4Wm−2). The uncertainties in radiative forcing due to aerosol radiative properties are estimated to be about 50 %. The aerosol in- direct effect is estimated to be of comparable magnitude to the direct forcing. We find that the magnitude of the forc- ing declined sharply from 1990 to 2010 (by 0.8Wm−2 di- rect and 1.0Wm−2 indirect), mainly reflecting decreases in SO2 emissions, and project that it will continue declining post-2010 but at a much slower rate since US SO2 emis- sions have already declined by almost 60% from their peak. This suggests that much of the warming effect of reducing US anthropogenic aerosol sources has already been realized. The small positive radiative forcing from US BC emissions (+0.3Wm−2 over the eastern US in 2010; 5% of the global forcing from anthropogenic BC emissions worldwide) sug- gests that a US emission control strategy focused on BC would have only limited climate benefit.
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