Cloud amounts from the International Satellite Cloud Climatology Project (I
SCCP) D-series data set and the TOVS Polar Pathfinder data set are compared
to surface observations of cloud amount from the North Polar (NP) drifting
station data set for the central Arctic. The results show that cloud obser
vations in the ISCCP data set differ significantly from surface observation
s and the annual cycle of cloudiness in the Arctic is reversed from what is
observed from the surface. In contrast, cloud amounts provided by the TOVS
Polar Pathfinder data set represent the annual cycle of cloudiness well. P
ath-P cloud retrievals also correspond well with surface observations (NP)
at timescales greater than 4 days.