Articles | Volume 18, issue 2
https://doi.org/10.5194/amt-18-327-2025
https://doi.org/10.5194/amt-18-327-2025
Research article
 | 
21 Jan 2025
Research article |  | 21 Jan 2025

Aerosol layer height (ALH) retrievals from oxygen absorption bands: intercomparison and validation among different satellite platforms, GEMS, EPIC, and TROPOMI

Hyerim Kim, Xi Chen, Jun Wang, Zhendong Lu, Meng Zhou, Gregory R. Carmichael, Sang Seo Park, and Jhoon Kim

Data sets

Absorbing Aerosol Optical Central Height (AOCH) retrieved from TROPOMI with UIowa's AOCH-O2AB algorithm Xi Chen https://doi.org/10.5281/zenodo.10407271

DSCOVR EPIC Aerosol Optical Centroid Height NASA/LARC/SD/ASDC https://doi.org/10.5067/EPIC/DSCOVR/L2_AOCH.001

GEMS Level2 AEH V2.0 and AERAOD V2.0 National Institute of Environmental Research Environmental Satellite Center https://nesc.nier.go.kr/en/html/datasvc/index.do

CALIPSO Lidar Level 2 Aerosol Profile, V4-21 NASA/LARC/SD/ASDC https://doi.org/10.5067/CALIOP/CALIPSO/CAL_LID_L2_05kmAPro-Standard-V4-21

CALIPSO Lidar Level 2 Aerosol Profile, V4-51 NASA/LARC/SD/ASDC https://doi.org/10.5067/CALIOP/CALIPSO/CAL_LID_L2_05kmAPro-Standard-V4-51

Model code and software

hkim144/ALH_comparison: ALH comparison (v0.1-beta) Hyerim Kim https://doi.org/10.5281/zenodo.10408292

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Short summary
We compare passive aerosol layer height (ALH) retrievals from the Earth Polychromatic Imaging Camera (EPIC), TROPOspheric Monitoring Instrument (TROPOMI), and Geostationary Environment Monitoring Spectrometer (GEMS) with lidar. GEMS shows a lower correlation (R = 0.64) than EPIC and TROPOMI (R > 0.7) but with minimal bias (0.1 km vs. overestimated by ~0.8 km). GEMS performance is improved for an ultraviolet aerosol index ≥ 3. EPIC and GEMS ALH diurnal variation differs slightly.