EO:EUM:DAT:0103
 TROPOMI Level 2 Aerosol Layer Height Products in NRT - Sentinel-5P
TROPOMI Level 2 Aerosol Layer Height Products in NRT - Sentinel-5PThe Aerosol Layer Height (ALH) is a new product with little heritage focusing on the
         retrieval of vertically localized aerosol layers in the free troposphere. Aerosol
         vertical profile products exist from other satellite instruments, e.g. Caliop on CALIPSO
         and MISR on Terra. The Aerosol Index described here is providing the air pressure
         at the center of the aerosol layer and the height at the center relative to the geoid.
         
         The retrieval of aerosol height is based on absorption by oxygen in the A band, based
         in near-infrared between 759 and 770 nm. This range is a highly structured line absorption
         spectrum with the strongest absorption lines occurring between 760 and 761 nm; the
         bands span a wide range of absorption optical thicknesses.
         
         First validation shows that the ALH is stable and shows good overall agreement with
         the Caliop retrievals, with TROPOMI generally showing lower ALH compared to Caliop
         over ocean scenes. The bias of the product can be up to a few hundred meters, but
         this is still under investigation. The product is very sensitive to cloud contamination
         and the height will be strongly biased towards the cloud height for partially clouded
         pixels. Furthermore, the product becomes unreliable for increasing surface albedo
         such as over deserts, biasing the ALH towards the surface.
         
         Finally, this product also helps to interpret the UV Aerosol Index (UVAI) in terms
         of aerosol absorption, as the index is strongly height-dependent.
         
         
Satellite: Sentinel-5P
         
         
Instrument: TROPOMI
         
         
Temporal Extent: 2025-05-27 -
         					
         						now
         					
         
         
Orbit Type: LEO
         
         
Data Policy: Copernicus
         
         
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