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                   3.  Stratus Clouds

               At times when conditions are favorable for fog, a very low cloud layer may form. This is
               especially true over flat terrain. These fog-like clouds form in stable air and often exist
               together with fog. When this happens, there is no exact point where it can be said that the
               fog layer stops and the stratus cloud layer begins. An observer on the surface then reports
               the vertical visibility as the distance he can see upward into the fog.
                   4.   Haze and Smoke


               Visibility is reduced when a stable layer of air contains large amounts of very small dust or
               salt particles. The particles produce the condition called haze. The haze may occasionally
               extend from the surface up to 15,000 feet. Haze layers often have definite upper 1imits or
               tops, above which air-to-air visibility is good. However, air-to-ground visibility from above a
               haze layer is poor, especially on a slant. Smoke restricts visibility in a manner similar to haze.
               Smoke sometimes collects in layers aloft, restricting visibility at that altitude, while visibility
               under it and over it may be good. Haze and smoke wil1 normally be a more severe restriction
               to visibility when a temperature inversion exists.

                   5.  Blowing Snow, Dust, and Sand

               ong surface winds and vertical currents in unstable air carry a erials from the surface such as
               dust, sand, or snow. These I reduce surface visibility to near zero over large areas. I favorable
               conditions dust can be carried aloft to 15,000 feet and restrict slant, flight, and surface
               visibility. Sand and snow are seldom carried aloft beyond a few hundred feet.

                         6.    Precipitation

                Snow, drizzle, and rain are the most common forms of precipitation that cause restrictions to
               visibility. Of these, snow is usually the most effective in reducing visibility. Heavy snow
               frequently reduces surface and slant visibility to near zero. Rain rarely reduces surface
               visibility to less than one mile and has a tendency to wash dust, smoke, and even fog particles
               out of the air. However, drizzle often occurs at the same time fog, haze, and smoke are
               present, resulting in visibility being less than it would be if rain had occurred. Precipitation on
               the windows of an aircraft greatly reduces a pilot's visibility; and if it freezes, he may have no
               forward visibility at all.
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