Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
Geoscience and Remote Sensing, Delft university of Technology (TU Delft), Mekelweg 2, 2628 CD, Delft, the Netherlands
Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
Mark ter Linden
Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
Geoscience and Remote Sensing, Delft university of Technology (TU Delft), Mekelweg 2, 2628 CD, Delft, the Netherlands
Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
Pieternel F. Levelt
Geoscience and Remote Sensing, Delft university of Technology (TU Delft), Mekelweg 2, 2628 CD, Delft, the Netherlands
Research and Development of Satellite Observations, Royal Netherlands Meteorological Institute (KNMI), Utrechtseweg 297, 3731 GA, De Bilt, the Netherlands
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This paper presents a first validation of the TROPOspheric Monitoring Instrument (TROPOMI) aerosol layer height (ALH) product, which is an estimate of the height of an aerosol layer using a spectrometer on board ESA's Sentinel-5 Precursor satellite mission. Comparison between the TROPOMI ALH product and co-located aerosol extinction heights from the CALIOP instrument on board NASA's CALIPSO mission show good agreement for selected cases over the ocean and large differences over land.
This paper presents a first validation of the TROPOspheric Monitoring Instrument (TROPOMI)...
