Anthropogenic aerosols: Indirect warming effect from dispersion forcing

[1]  G. McFarquhar,et al.  Parameterizations of INDOEX microphysical measurements and calculations of cloud susceptibility: Applications for climate studies , 2001 .

[2]  J. Hudson,et al.  Maritime-Continental Drizzle Contrasts in Small Cumuli , 2001 .

[3]  J. Hudson,et al.  Microphysical relationships in warm clouds , 2001 .

[4]  Jonathan P. Taylor,et al.  Effects of Aerosols on Cloud Albedo: Evaluation of Twomey's Parameterization of Cloud Susceptibility Using Measurements of Ship Tracks. , 2000 .

[5]  Jonathan P. Taylor,et al.  A Case Study of Ship Track Formation in a Polluted Marine Boundary Layer , 2000 .

[6]  Jonathan P. Taylor,et al.  A Case Study of Ships Forming and Not Forming Tracks in Moderately Polluted Clouds , 2000 .

[7]  P. Daum,et al.  Spectral dispersion of cloud droplet size distributions and the parameterization of cloud droplet effective radius , 2000 .

[8]  J. Hudson,et al.  Droplet Spectral Broadening in Marine Stratus , 1997 .

[9]  J. Hudson,et al.  Microphysical Contrasts in Atlantic Stratus , 1995 .

[10]  P. Hobbs,et al.  Long-range transport of continental aerosols over the Atlantic Ocean and their effects on cloud structures , 1995 .

[11]  D. W. Johnson,et al.  The Measurement and Parameterization of Effective Radius of Droplets in Warm Stratocumulus Clouds , 1994 .

[12]  J. Coakley,et al.  Climate Forcing by Anthropogenic Aerosols , 1992, Science.

[13]  V. R. Noonkester,et al.  Droplet Spectra Observed in Marine Stratus Cloud Layers , 1984 .

[14]  S. Twomey Pollution and the Planetary Albedo , 1974 .