NOAA Office of Satellite and Product Operations

SPECIAL MESSAGE:

GOES-13 Sounder IR data is not available. All products from GOES-13 (GOES-East) Sounder IR data have been halted and distribution has been stopped except the Sounder ASOS SCP products for CONUS, which are replaced with GOES-East Imager ASOS SCP products for CONUS. Engineers are investigating the problem.

GVI - Precipitable Water Index

The Precipitable Water Index (PWI), otherwise known as the brightness temperature difference, is the difference between AVHRR channels 4 and 5. PWI is a measurement of how much water vapor is in the atmosphere (lower K values denote higher concentrations of water vapor). Since AVHRR channels 4 and 5 are volume sampled from the top of the atmosphere to the surface, PWI, to an extent, measures the total column precipitable water in the atmosphere (Steve Olson, 1997).


GVI Precipitable Water Index image

Regions on display include North America, South America, Alaska, Europe, Asia,
British Isles, Africa, and Oceania.

Please note that PWI is not the same as relative humidity, which measures the percentage of water vaper over the amount of water vapor needed for saturation at a given temperature.