Aerosol Optical Properties Affected by a Strong Dust Storm over Central and Northern China

Aerosol observational data at 8 ground-based observation sites in the Chinese Sun Hazemeter Network(CSHNET)were analyzed to characterize the optical properties of aerosol particles during the strong dust storm of 16-21 April 2005.The observational aerosol optical depth(AOD)increased significantly during this dust storm at sites in Beijing city(86%),Beijing forest(84%),Xianghe(13%),Shapotou(27%),Shenyang(47%),Shanghai(23%),and Jiaozhou Bay(24%).The API(air pollution index)in Beijing and Tianjin also had a similar rise during the dust storm,while the Angstrm exponent(α)declined evidently at sites in Beijing city(21%),Beijing forest(39%),Xianghe(19%),Ordos(77%),Shapotou(50%),Shanghai(12%),and Jiaozhou Bay(21%),respectively.Furthermore,The observational AOD andαdemonstrated contrary trends during all storm stages(pre-dust storm,dust storm,and post-dust storm),with the AOD indicating an obvious"Valley-Peak-Valley"pattern of variation,whileαdemonstrated a"Peak-Valley-Peak"pattern. In addition,the dust module in a regional climate model(RegCM3)simulated the dust storm occurrence and track accurately and RegCM3 was able to basically simulate the trends in AOD.The simulation results for the North China stations were the best,and the simulation for dust-source stations was on the high side,while the simulation was on the low side for coastal sites.

Aerosol Optical Properties Affected by a Strong Dust Storm over Central and Northern China

Aerosol observational data at 8 ground-based observation sites in the Chinese Sun Hazemeter Network (CSHNET) were analyzed to characterize the optical properties of aerosol particles during the strong dust storm of 16--21 April 2005. The observational aerosol optical depth (AOD) increased significantly during this dust storm at sites in Beijing city (86%), Beijing forest (84%), Xianghe (13%), Shapotou (27%), Shenyang (47%), Shanghai (23%), and Jiaozhou Bay (24%). The API (air pollution index) in Beijing and Tianjin also had a similar rise during the dust storm, while the Angstrom exponent (alpha) declined evidently at sites in Beijing city (21%), Beijing forest (39%), Xianghe (19%), Ordos (77%), Shapotou (50%), Shanghai (12%), and Jiaozhou Bay (21%), respectively. Furthermore, The observational AOD and alpha demonstrated contrary trends during all storm stages (pre-dust storm, dust storm, and post-dust storm), with the AOD indicating an obvious ``Valley--Peak--Valley' pattern of variation, while alpha demonstrated a ``Peak--Valley-- Peak' pattern. In addition, the dust module in a regional climate model (RegCM3) simulated the dust storm occurrence and track accurately and RegCM3 was able to basically simulate the trends in AOD. The simulation results for the North China stations were the best, and the simulation for dust-source stations was on the high side, while the simulation was on the low side for coastal sites.