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Dear GES DISC,

Thank you for maintaining a great data portal. I am interested in using Giovanni AAOD data , and I wonder about the artificial division between the SH and NH apparent at the Equator for AAOD500 and AAOD388?
Any feedback on this would be great, thanks.

 

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  1. The sharp gradient you have observed is associated with a hemisphere-dependent
    threshold in AIRS CO that we use in the aerosol type identification. That has
    been corrected in a new version of the OMAERUV  to be released soon. What
    period and region are you looking at?  If interested, I can make available to
    you gridded monthly values of the upcoming data.  
     
    Omar Torres
     
    NASA-GSFC