A. S. Ackerman, O. B. Toon, and P. V. Hobbs, A model for particle microphysics,
turbulent mixing, and radiative transfer in the stratocumulus-topped marine
boundary layer and comparisons with measurements, J. Atmos. Sci. 52,
1204-1236, 1995
The first integral in eqn. 1 should be multiplied by 1/2.
The right hand side of eqn. 2 should be replaced with 4 pi rhow
times an integral over droplet radius of r2 gr(r) C(r) dr
The term ( g1 g2 qrad ) in eqn. 3 should
be subtracted, not added.
The right hand side of eqn. C2 should be preceded by a minus sign.
A. S. Ackerman, O. B. Toon, D. E. Stevens, A. J. Heymsfield, V. Ramanathan,
and E. J. Welton, Reduction of tropical cloudiness by soot, Science 288,
1042-1047, 2000
In the second complete paragraph on p. 1045, the clear-sky forcing
is -3.0 W/m2, not 3.0 W/m2 as stated (note that the
logic of of the preceding sentence in the paragraph only makes sense with
this sign convention).
The Stevens and Bretherton citation in reference 17 was published in
1996, not 1997 as stated.
R. J. Charlson, A. S. Ackerman, F. A.-M. Bender, T. L. Anderson, and Z. Liu,
On the climate forcing consequences of the albedo continuum between cloudy
and clear air. Tellus 59B, 715-727, 2007
The geometric standard deviation used for the dry aerosol size distribution
was 1.5 not 1.2 as stated.