Articles | Volume 11, issue 7
https://doi.org/10.5194/amt-11-4509-2018
https://doi.org/10.5194/amt-11-4509-2018
Research article
 | 
27 Jul 2018
Research article |  | 27 Jul 2018

The importance of surface reflectance anisotropy for cloud and NO2 retrievals from GOME-2 and OMI

Alba Lorente, K. Folkert Boersma, Piet Stammes, L. Gijsbert Tilstra, Andreas Richter, Huan Yu, Said Kharbouche, and Jan-Peter Muller

Viewed

Total article views: 4,038 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,686 1,250 102 4,038 381 103 94
  • HTML: 2,686
  • PDF: 1,250
  • XML: 102
  • Total: 4,038
  • Supplement: 381
  • BibTeX: 103
  • EndNote: 94
Views and downloads (calculated since 07 Mar 2018)
Cumulative views and downloads (calculated since 07 Mar 2018)

Viewed (geographical distribution)

Total article views: 4,038 (including HTML, PDF, and XML) Thereof 3,838 with geography defined and 200 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Short summary
Light reflected by Earth’s surface is different in each direction: it appears brighter or darker in certain viewing directions. Currently this effect is not accounted for in satellite retrievals; thus surface reflectance climatologies and cloud fractions show an east-west bias across orbits (GOME2,OMI). The effect for NO2 measurements in partly cloudy scenes is substantial. We recommend that this effect in UV/Vis sensors coherently accounted for, and will be especially beneficial for TROPOMI.