Tuesday, August 20, 2019
Storms :: essays research papers
 If you know where and when to look, you can  treat yourself to a colourful display of atmospheric  haloes, spots and pillars. These images can tell you  something about the clouds overhead and possible  changes in the weather. All of these images are  created by light shining through cirrostratus clouds.  These clouds occur at an altitude of 6,000-12,000  metres. They appear as a thin sheet or layer  (strata) that is pure white. The layer of cloud is so  thin (only 100-450 metres) that is doesn't obscure  the sun or moon, so you should be able to see  your shadow. Cirrostratus is made of many types  of ice crystals. However, four crystal shapes are  responsible for producing most of the commonly  see haloes-plate crystals, columns, capped  columns and bullets. The most obvious halo is  found around the sun. If the layer of cirrostratus is  extensive, you'll see an entire ring. Within the layer  of cloud, sunlight is striking and passing through  the sides of randomly-oriented ice crystals. As the  sunlight passes through each crystal, the light  changes direction, or refracts. The radius of the  hale depends on the amount of change in the  direction of the sun's light. Usually this is 22  degrees. Since the sun is 1/2 of a degree across,  the radius of the halo is 44 sun-widths.  Occasionally you may see a second halo at 46  degrees from the sun (that is, with a radius of 92  sun-widths). This is produced by sunlight passing  through both the side and bottom of each crystal.  Moonlight will also produce a halo, around the  moon, with the proper layer of cirrostatus.  Another common optical effect is known as "mock  suns" or "sun dogs" or "parhelia" (Greek for "with  the sun"). These bright spots on either side of the  sun, outside of the halo, occur when sunlight  passes through the sides of capped columns,  bullets and plate crystals, when these crystals are  arranged with their sides vertical. The crystals  wobble, diffusing and smearing the colours of the  mock sun. You can see haloes and mock suns  more clearly if you block out your view of the real  sun by holding your hand in front of it at arm's  length. Another spectactular optical effect is the  solar pillar. This is a vertical shaft of light the same  colour as the sun stretching upwards from the sun  and is most often seen at sunset or sunrise. It's  produced by sunlight reflecting of the base of plate  and capped column crystals in the clouds.  					    
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