component, leaving only that which has been reflected by the sun. Because liquid water clouds are more reflective than ice clouds at 3.9 um, this product may be used for daytime cloud phase determination. A more complete
description of the reflectivity product and its applications may be found in the RAMM Teams's 3.9 um tutorial. (Make sure you "bookmark" this location if you wish to return here from the tutorial!)
With the enhancement shown, the reflectivity product displays liquid water clouds as bright, and clouds comprised of ice crystals as dark. Cloud phase differentiation is important since lightning will not be present unless glaciation has occurred.
If you came to this page from the "Sub-synoptic-scale IR (3.9 um) Imagery" presentation, and wish to return there, click here.