Surrounding "weather" cloud cover was minimal at this time allowing for easy discrimination of the ash cloud. Had colder cloud tops been present nearby, the 11-µm channel data alone might not have been able to differentiate between ash and water clouds. Inspection of the color-enhanced 11-µm image shows the extent of the ash plume from the Mt. Spurr eruption on 19 September 1992 at 5:12 UTC (21:12 local time). Notice that the size, shape, and temperature of the plume could be mistaken as the top of an anvil cloud associated with a strong convective cell.
Could the use of multispectral processing techniques improve discrimination of ash from water clouds? Go to the next page for an example.