Comment on “Control of fossil‐fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming” by M. Z. Jacobson

[1]  S. Twomey.  The Influence of Pollution on the Shortwave Albedo of Clouds , 1977 .

[2]  C. Liousse,et al.  Construction of a 1° × 1° fossil fuel emission data set for carbonaceous aerosol and implementation and radiative impact in the ECHAM4 model , 1999 .

[3]  V. Ramanathan,et al.  Evidence of surface cooling from absorbing aerosols , 2002 .

[4]  D. Randall,et al.  A cumulus parameterization with multiple cloud base levels , 1998 .

[5]  J. Burt,et al.  Magnitude of ocean temperature feedback effects in a coupled carbon-budget energy-balance model for the period 1800–2100 , 1980 .

[6]  M. Jacobson.  A physically‐based treatment of elemental carbon optics: Implications for global direct forcing of aerosols , 2000 .

[7]  Andrei P. Sokolov,et al.  Quantifying Uncertainties in Climate System Properties with the Use of Recent Climate Observations , 2002, Science.

[8]  Gabriele C. Hegerl,et al.  A Comparison of Surface Air Temperature Variability in Three 1000-Yr Coupled Ocean–Atmosphere Model Integrations , 2000 .

[9]  T. Wigley,et al.  Natural variability of the climate system and detection of the greenhouse effect , 1990, Nature.

[10]  T. Barnett,et al.  Unforced decadal fluctuations in a coupled model of the atmosphere and ocean mixed layer , 1992 .

[11]  W. Gates.  AMIP: The Atmospheric Model Intercomparison Project. , 1992 .

[12]  B. Albrecht.  Aerosols, Cloud Microphysics, and Fractional Cloudiness , 1989, Science.

[13]  Leon D. Rotstayn,et al.  Indirect Aerosol Forcing, Quasi Forcing, and Climate Response , 2001 .

[14]  V. Ramaswamy,et al.  A general circulation model study of the global carbonaceous aerosol distribution , 2002 .

[15]  M. Jacobson.  Numerical Techniques to Solve Condensational and Dissolutional Growth Equations When Growth is Coupled to Reversible Reactions , 1997 .

[16]  Barbara J. Turpin,et al.  Species Contributions to PM2.5 Mass Concentrations: Revisiting Common Assumptions for Estimating Organic Mass , 2001 .

[17]  M. Jacobson.  GATOR-GCMM: A global through urban scale air pollution and weather forecast model , 2001 .

[18]  M. Jacobson,et al.  Strong radiative heating due to the mixing state of black carbon in atmospheric aerosols , 2022 .

[19]  R. Sausen,et al.  Stratosphere adjusted radiative forcing calculationsin a comprehensive climate model , 2001 .

[20]  Syukuro Manabe,et al.  Low-Frequency Variability of Surface Air Temperature in a 1000-Year Integration of a Coupled Atmosphere-Ocean-Land Surface Model , 1996 .

[21]  S. M. Marlais,et al.  An Overview of the Results of the Atmospheric Model Intercomparison Project (AMIP I) , 1999 .

[22]  S. Schneider,et al.  Volcanic Dust, Sunspots, and Temperature Trends , 1975, Science.

[23]  A. Callegari,et al.  The role of deep sea heat storage in the secular response to climatic forcing , 1980 .

[24]  Ulrike Lohmann,et al.  Erratum: ``Prediction of the number of cloud droplets in the ECHAM GCM'' , 1999 .

[25]  Joyce E. Penner,et al.  Soot and smoke aerosol may not warm climate , 2002 .

[26]  J. Hansen,et al.  Radiative forcing and climate response , 1997 .

[27]  Joyce E. Penner,et al.  Indirect effect of sulfate and carbonaceous aerosols: A mechanistic treatment , 2000 .

[28]  Ulrike Lohmann,et al.  Can the direct and semi‐direct aerosol effect compete with the indirect effect on a global scale? , 2001 .

[29]  J. Hansen,et al.  Global warming in the twenty-first century: an alternative scenario. , 2000, Proceedings of the National Academy of Sciences of the United States of America.

[30]  M. Jacobson.  Control of fossil‐fuel particulate black carbon and organic matter, possibly the most effective method of slowing global warming , 2002 .

[31]  J. Seinfeld,et al.  Global distribution and climate forcing of carbonaceous aerosols , 2002 .

[32]  J. Hansen,et al.  Climate Response Times: Dependence on Climate Sensitivity and Ocean Mixing , 1985, Science.

[33]  J. Penner,et al.  Cloud susceptibility and the first aerosol indirect forcing: Sensitivity to black carbon and aerosol concentrations , 2002 .

[34]  C. Hewitt,et al.  The impact of dynamic sea-ice on the climatology and climate sensitivity of a GCM: a study of past, present, and future climates , 2001 .

[35]  Inez Y. Fung,et al.  Global climate changes as forecast by Goddard Institute for Space Studies three‐dimensional model , 1988 .