Journal
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
Volume 115, Issue -, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2009JD013481
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- INSA
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The number size distributions of aerosol particles in the size-range of 0.003-20 mu m diameter have been measured at Maitri (70 degrees 45' 52 '' S, 11 degrees 44' 03 '' E, 117m above mean sea level), Antarctica, when two circumpolar cyclonic storms passed close to the station during February, 2005. As a storm approaches toward Maitri, concentration of coarse particles increases by about an order of magnitude and the number size-distribution frequently shows a coarse mode at similar to 2 mu m, a broad Aitken mode from 0.04 to 0.1 mu m and, occasionally, a nucleation mode at 0.018 mu m diameter. When the storm is going away from Maitri, in addition to the coarse mode at similar to 2 mu m and a peak at 0.08 mu m diameter, a nucleation mode frequently appears at < 0.01 mu m diameter and the mode existing at 0.018 mu m diameter shifts to 0.02-0.04 mu m diameter. Particles in the range of 0.008-0.03 mu m diameter grow at the rate of 0.2-0.6 nm h(-1) in the case of Storm I, but no appreciable growth is observed in the case of Storm II. The peak at 0.02-0.04 mu m is often so dominant that it envelops the peak at 0.08 mu m diameter. Results are interpreted in terms of the mixing of continental and oceanic air masses with the subsidence associated with the storm. The nucleation mode at 0.01 mu m diameter has been associated with the new particles formed in the outflow at the top of clouds and the coarse mode at 2 mu m diameters with the re-suspension of particles from the surface.
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