Black carbon and brown clouds

In aerosol hot spots around the globe, solar radiation is dimmed down on its way to the Earth's surface. The resulting surface cooling turns out to be almost in balance with heating of the atmosphere due to black carbon.

[1]  Michael Schulz,et al.  Radiative forcing by aerosols as derived from the AeroCom present-day and pre-industrial simulations , 2006 .

[2]  John H. Seinfeld,et al.  Climate response of direct radiative forcing of anthropogenic black carbon , 2005 .

[3]  Vincent R. Gray Climate Change 2007: The Physical Science Basis Summary for Policymakers , 2007 .

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

[5]  Martin Wild,et al.  Inaugural Article by a Recently Elected Academy Member , 2003 .

[6]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[7]  Tami C Bond,et al.  Can reducing black carbon emissions counteract global warming? , 2005, Environmental science & technology.

[8]  P. S. Praveen,et al.  Atmospheric brown clouds: Hemispherical and regional variations in long‐range transport, absorption, and radiative forcing , 2007 .

[9]  J. Hansen,et al.  Climate Effects of Black Carbon Aerosols in China and India , 2002, Science.

[10]  Olivier Boucher,et al.  Aerosol absorption and radiative forcing , 2006 .

[11]  S. Satheesh Aerosol radiative forcing over land: effect of surface and cloud reflection , 2002 .

[12]  J. Kiehl,et al.  Atmospheric brown clouds: impacts on South Asian climate and hydrological cycle. , 2005, Proceedings of the National Academy of Sciences of the United States of America.

[13]  P. S. Praveen,et al.  Understanding the origin of black carbon in the atmospheric brown cloud over the Indian Ocean , 2007 .