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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, D11109, doi:10.1029/2007JD009152, 2008

Multimodel projections of climate change from short-lived emissions due to human activities

Drew T. Shindell

NASA Goddard Institute for Space Studies, New York, New York, USA


Hiram Levy II

NOAA Geophysical Fluid Dynamics Laboratory, Princeton University, Princeton, New Jersey, USA


M. Daniel Schwarzkopf

NOAA Geophysical Fluid Dynamics Laboratory, Princeton University, Princeton, New Jersey, USA


Larry W. Horowitz

NOAA Geophysical Fluid Dynamics Laboratory, Princeton University, Princeton, New Jersey, USA


Jean-Francois Lamarque

Atmospheric Chemistry Division, National Center for Atmospheric Research, Boulder, Colorado, USA


Greg Faluvegi

NASA Goddard Institute for Space Studies, New York, New York, USA


Abstract

We use the GISS (Goddard Institute for Space Studies), GFDL (Geophysical Fluid Dynamics Laboratory) and NCAR (National Center for Atmospheric Research) climate models to study the climate impact of the future evolution of short-lived radiatively active species (ozone and aerosols). The models used mid-range A1B emission scenarios, independently calculated the resulting composition change, and then performed transient simulations to 2050 examining the response to projected changes in short-lived species and to changes in both long-lived and short-lived species together. By 2050, two models show that the global mean annual average warming due to long-lived GHGs (greenhouse gases) is enhanced by 20–25% due to the radiatively active short-lived species. One model shows virtually no effect from short-lived species. Intermodel differences are largely related to differences in emissions projections for short-lived species, which are substantial even for a particular storyline. For aerosols, these uncertainties are usually dominant, though for sulfate uncertainties in aerosol physics are also substantial. For tropospheric ozone, uncertainties in physical processes are more important than uncertainties in precursor emissions. Differences in future atmospheric burdens and radiative forcing for aerosols are dominated by divergent assumptions about emissions from South and East Asia. In all three models, the spatial distribution of radiative forcing is less important than that of climate sensitivity in predicting climate impact. Both short-lived and long-lived species appear to cause enhanced climate responses in the same regions of high sensitivity rather than short-lived species having an enhanced effect primarily near polluted areas. Since short-lived species can significantly influence climate, regional air quality emission control strategies for short-lived pollutants may substantially impact climate over large (e.g., hemispheric) scales.

Received 25 June 2007; accepted 6 February 2008; published 6 June 2008.

Keywords: Climate; aerosols; ozone.

Index Terms: 1610 Global Change: Atmosphere (0315, 0325); 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801, 4906); 1637 Global Change: Regional climate change; 0365 Atmospheric Composition and Structure: Troposphere: composition and chemistry; 3305 Atmospheric Processes: Climate change and variability (1616, 1635, 3309, 4215, 4513).

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Citation: Shindell, D. T., H. Levy II, M. D. Schwarzkopf, L. W. Horowitz, J.-F. Lamarque, and G. Faluvegi (2008), Multimodel projections of climate change from short-lived emissions due to human activities, J. Geophys. Res., 113, D11109, doi:10.1029/2007JD009152.