• Jacobson, M. Z., 2002: Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming. J. Geophys. Res., 107 .4410, doi:10.1029/2001JD001376.

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  • Jacobson, M. Z., 2003a: Reply to comment by J. Feichter et al. on “Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming.’’. J. Geophys. Res., 108 .4768, doi:10.1029/2002JD003299.

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  • Jacobson, M. Z., 2003b: Reply to comment by J. E. Penner on “Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming.’’. J. Geophys. Res., 108 .4772, doi:10.1029/2003JD003403.

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  • Jacobson, M. Z., 2003c: Reply to comment by D. P. Chock et al. on “Control of fossil-fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming.’’. J. Geophys. Res., 108 .4770, doi:10.1029/2003JD003707.

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  • Jacobson, M. Z., 2004: Climate response of fossil-fuel and biofuel soot, accounting for soot’s feedback to snow and sea ice albedo and emissivity. J. Geophys. Res., 109 .D21201, doi:10.1029/2004JD004945.

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  • Johnson, B. T., 2005: The semidirect effect: Comparisons of a single-column model with large eddy simulation for marine stratocumulus. J. Climate, 18 , 119130.

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  • 1 Department of Civil and Environmental Engineering, Stanford University, Stanford, California
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Corresponding author address: Dr. Mark Z. Jacobson, Terman Engineering Center, M-31, Stanford University, Stanford, CA 94305-4020. Email: jacobson@stanford.edu

Corresponding author address: Dr. Mark Z. Jacobson, Terman Engineering Center, M-31, Stanford University, Stanford, CA 94305-4020. Email: jacobson@stanford.edu

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