To evaluate the MODIS cloud product we employed the cloud detection algorithm SPARC (Separation of Pixels using Aggregated Rating over Canada) developed at the Canada Centre for Remote Sensing. SPARC is able to produce alternative cloud masks, cloud top height estimation, and other parameters. It was found that agreement between MODIS and SPARC cloud masks is on average around 74% and up to 86% during summer. The total percentage of the pixels that were mistakenly identified as clear-sky by one scheme and overcast cloudy by another scheme was less than 2%.
As MODIS cloud detection is designed to be clear-sky conservative, i.e. sensitive to any indication of cloud contamination (real or false), it may sometimes identify haze or inhomogeneous snow covered surface in the boreal zone as overcast cloud. This may turn cloud flags on and initiate cloud property retrievals assuming dark surface underneath. We analyzed a number of such situations to determine the overall impact on cloud statistics and radiative fluxes for CloudSat observational conditions and general geometry.
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