Figure 6
HSRL vertical profiles featuring complex layering of aerosol particles and dust transport. Atmospheric backscatter cross-section at 532 nm (a) and linear depolarization (b) observed by the HSRL in Seoul during a period featuring complex aerosol vertical profiles driven by dynamic meteorology (04–05 May 2016). Altitude is provided above mean sea-level (MSL), which is an approximate AGL altitude (Seoul 38 m MSL). The approximate duration of each NASA DC-8 science flight is denoted by a brown arrow. DOI: https://doi.org/10.1525/elementa.395.f6

HSRL vertical profiles featuring complex layering of aerosol particles and dust transport. Atmospheric backscatter cross-section at 532 nm (a) and linear depolarization (b) observed by the HSRL in Seoul during a period featuring complex aerosol vertical profiles driven by dynamic meteorology (04–05 May 2016). Altitude is provided above mean sea-level (MSL), which is an approximate AGL altitude (Seoul 38 m MSL). The approximate duration of each NASA DC-8 science flight is denoted by a brown arrow. DOI: https://doi.org/10.1525/elementa.395.f6

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