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The NASA space-borne Mie-lidar system CALIPSO/CALIOP revealed that multiplelarge Asian dust layers with a horizontal scale of 2000–3000 km reachedNorth America, occupying the full troposphere, in April 2010. This kind ofdust layer transport has not been reported before. Our analysis of CALIOPdata and global aerosol model results revealed that frequent dust emissionsoccurred in northwestern China because of stronger-than-average near-surfacewinds, and that strong stable westerly winds carried the Asian dust fromnorthwestern China to the central Pacific Ocean. A negative pressure anomalywas located in the eastern Pacific Ocean, and the main dust transport pathwas split into two branches: a northern path and a southern path over NorthAmerica. Northern-path dust was trapped and stagnant for a longer time thansouthern path dust and finally subsided under a high-pressure system. Dustalong the southern path reached the central US. These complex conditionsresulted in a multi-layered structure of dust over North America

Large Asian dust layers continuously reached North America in April 2010