Physical properties of the aerosol at the South Pole

Mathematics – Logic

Scientific paper

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Aerosols, Antarctic Regions, Particle Size Distribution, Physical Properties, Ground Stations, Hygroscopicity, Meteorological Parameters, Particle Motion

Scientific paper

The size distribution of aerosol arriving at the South Pole was measured several times during four days of relatively homogeneous meteorological transport conditions. This aerosol had a maximum number concentration in the 0.000001-0.000008 cm radius range, and a maximum volume concentration in the 0.00002-0.0002 cm radius range, a total number concentration of 106/cu cm and a total volume concentration of 0.000001 cu cm/cu m. Almost all particles of r approximately equal to 0.00015 cm were hygroscopic, with refractive index near 1.54. This aerosol represents the background aerosol which occurs at the end point of a long series of meteorological precipitation processes.

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