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http://dx.doi.org/10.7780/kjrs.2014.30.6.5

Long-Range Transported SO2 Inflow fromAsian Continent to Korea Peninsula Using OMI SO2 Data and HYSPLIT Backward Trajectory Calculations  

Park, Junsung (Department of Spatial Information Engineering, Pukyong National University)
Hong, Hyunkee (Department of Spatial Information Engineering, Pukyong National University)
Choi, Wonei (Department of Spatial Information Engineering, Pukyong National University)
Lee, Hanlim (Department of Spatial Information Engineering, Pukyong National University)
Publication Information
Korean Journal of Remote Sensing / v.30, no.6, 2014 , pp. 743-754 More about this Journal
Abstract
In this present paper, we, for the first time, calculated $SO_2$ inflow from China to Korea peninsula based on OMI $SO_2$ products and HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory Model) backward trajectory calculations. The major factors used to estimate $SO_2$ flux are long range transported $SO_2$ concentration, transport speed of air mass, and thickness of transported air mass layer. The mean and maximum $SO_2$ fluxes are estimated to be 0.81 and $2.11g{\cdot}m^{-2}{\cdot}h^{-1}$, respectively based on OMI products while, those of $SO_2$ fluxes are 0.50 and $1.18g{\cdot}m^{-2}{\cdot}h^{-1}$ respectively using insitu data obtained at the surface. For most cases, larger $SO_2$ inflow values were found at the surface than those estimated for the air mass layer which extends from surface up to 1.5 km. However, increased transport speed of air mass leads to the enhanced $SO_2$ flux at the altitude up to 1.5 km at the receptor sites. Additionally, we calculate uncertainties of $SO_2$ flux using error propagation method.
Keywords
$SO_2$ inflow; OMI; Long range transport;
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