Some Results of an Experimental Study of the Atmospheric Aerosol in Tomsk: A Combined Approach
نویسنده
چکیده
As widely accepted, the atmospheric aerosol strongly contributes to the formation of the earth’s radiation balance through the absorption and scattering of solar radiation. In addition to this direct influence on the radiation balance, aerosols, being active condensation nuclei, also have a role in the cloud formation processes. Consequently, we pay special attention to the block of aerosol studies in our Tomsk Radiation Experiment in Siberia (TRES) Project, proposed for the Atmospheric Radiation Measurement (ARM) Program.
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