The global distribution of supersaturation in the upper troposphere from the atmospheric infrared sounder

AIRS data compare well to other in situ and satellite observations of RH and provide daily global coverage up to 200 hPa, though satellite observations of supersaturation are highly uncertain. The climatology of supersaturation is analyzed statistically to understand where supersaturation occurs and how frequently.

Supersaturation occurs in humid regions of the upper tropical tropopause near convection 10%-20% of the time at 200 hPa. Supersaturation is very frequent in the extratropical upper troposphere, occurring 20%-40% of the time, and over 50% of the time in storm track regions below the tropopause. The annual cycle of supersaturation is consistent for the 2.5 yr of data analyzed.