NOAA-NESDIS
Regional And Mesoscale Meteorology Team
Daily Satellite Discussion
Tuesday December 16, 1997
Today's discussion looks at the use of the reflectivity product. The reflectivity product has several advantages because the reflectivity component of the 3.9 um IR imager channel is emphasized.

The loop shows the fog product for Tuesday afternoon 19Z- 22Z. Notice how well the fog in California shows up. The fog particles are more reflective at cloud top because they are comprised of water droplets which reflect more of the solar radaition at 3.9 than clouds composed of ice crystals or snow. The weather observations have been plotted on two images to show the extensive area of fog. Visibilities as low as one-tenth of a mile were reported in the fog in the interior valleys of California. Deadly car accidents have occurred in the last 3 weeks due to dense fog. NOTE:The areas around the northern Gulf of California in the Mexican Grand Desert exhibit a "false fog" signal in this product due to differences in the emissivity of the soils at 3.9 um and 10.7 um. For clarity, red braces highlight a false fog area and yellow braces highlight a real fog area.

Average image
(click to enlarge)
The loop was averaged to produce the average image shown above. Note that the surface features appear very sharp where the skies have been clear. In this case, much of the fog in the interior valley of California shows up quite nicely as there were not any significant clouds above the fog. You can also see fog in CO and UT. You can even see the fog extending into northern california through the cirrus cloud deck! Notice the areas that seem blurry. These areas are where clouds were moving during the time period. The cirrus tends to be the fastest moving cloud type and that is indicated in these images. Also notice the low cloud area over the eastern Dakotas, this cloud is less "blurred" as it was moving much slower than the high cirrus clouds. However, the clouds off the west coast of California do show a nice pattern indicating the low-level flow. The imagery is less blurred because the cumulus that formed moved slower than the cirrus. Finally, the last image shows the plotted (observed) visibility. Note the low visibility of .1 reported in southern CA.

Average image with surfac visibilities in miles.
(click to enlarge)

Brian Motta

We welcome your comments and discussion at ramsdis@comet.ucar.edu


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