The soil particle size dependent emission parameterization for an Asian dust (Yellow Sand) observed.pdf
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The soil particle size dependent emission parameterization for an Asian dust (Yellow Sand) observed
Atmospheric Environment 37 (2003) 4625–4636
ARTICLE IN PRESS
AE International – Asia*Correspondin
E-mail addre
1352-2310/$ - see
doi:10.1016/j.atmThe soil particle size dependent emission parameterization for
an Asian dust (Yellow Sand) observed in Korea in April 2002
Hee-Jin In, Soon-Ung Park*
School of Earth and Environmental Sciences, Seoul National University, San 56-1 Shilim-Dong, Kwanak-Ku, Seoul 151-742, South Korea
Received 3 April 2003; received in revised form 24 July 2003; accepted 30 July 2003Abstract
Intense Asian dust (Yellow Sand) events have been observed in Korea on 21–23 March and 7–9 April 2002. During
these periods the observed PM10 concentrations were over 1000mgm
3 at most monitoring sites in South Korea. The
operational meteorological model of the Regional Data Assimilation and Prediction System of the Korea
Meteorological Administration and the aerosol transport model with the improved particle size distribution
parameterization developed at Seoul National University were used to simulate the intense Yellow Sand event
observed on 7–9 April 2002. The comparison with the observational data shows that the present model system could
reasonably simulate the evolutionary features of Yellow Sand over South Korea including the starting and ending time
of the event, the particle size spectrum and the PM10 concentration. It was found that the dominant particle diameter in
the mass concentration ranged from 3.67 to 10mm during this dust event. A promising dust emission model depending
on the particle size distribution constructed by the sum of several log-normal distributions of particle sizes of different
soil types has been developed and found to yield better spectral-mass concentration in the size range of larger than
10mm. This result suggests that size distributions of Asian dust (Yellow Sand) are consistent with those found in the
USA, Central Asia and the Sahara desert. However, the accuracy of the model requires more detailed soil particle
dist
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