Abstract
Dust particles generated by wind erosion from northern China are an important source of atmospheric aerosols,exerting a profound influence on the atmospheric processes and global radiation balance. It is paid particular attention to the simulation of dust emissions from northern China in 2006. Highly-resolved MODIS( Moderate Resolution Imaging Spectroradiometer) land cover and NDVI( Normalized Difference Vegetation Index)data were included in the fifth-generation Mesoscale Model( MM5) to improve the model performance. Monthly MODIS NDVI were also utilized to quantify the suppression of vegetation growth on dust uplift. Approximately4. 36 × 109 t of dust particles between 0. 2 and 74 μm in diameter were released annually,characterized by a maximum load of 2. 64 × 109 t in spring. Four potential sources,including the Badanjilin desert,the gobi regions in northwestern Inner Mongolia and the Hexi Corridor,the sand-land in central Inner Mongolia,and the Takelamagan desert along with the adjacent regions,were identified as the dominant contributors in spring.
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