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CLASSIFICATION OF CLOUDS |
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Clouds are continuously in a process of change and appear, therefore in an infinite variety of forms. It is possible, however, to define a limited number of characteristic forms , frequently observed all over the world, into which clouds can be broadly grouped. A classification of the characteristic forms of clouds, in terms of "genera," "species" and "varities" has been established. Intermediate or transitional forms, although observed fairly frequently, have lesser longevity and their appearance is not very different from that indicated in the definitions of the characteristic forms. Finally, there exists a group of clouds, rarely or occasionally observed, not included in the following classification. Some of these "special clouds" consist for the greater part or in their entirety of non-aqueous liquid or solid particles. The definition of a cloud given above is therefore not applicable to all special clouds. Included in the "special" clouds are the nacreous clouds which by day resemble pale cirrus, but after sunset, are characterized by brilliant colors. They occur at altitudes between 21 and 30 kilometers (70,000 and 100,000 feet). The physical constitution of nacreous clouds is still unknown. However, the simultaneous occurrence of various diffraction colors in more or less irregular patterns indicates the presence of minute particles, possibly spherical ice particles. Noctilucent clouds also resemble thin cirrus, but usually with a bluish or silvery, or sometimes orange to red color; they stand out against the dark sky. Measurements have shown that their altitude ranges from 75 to 90 kilometers (250,000 to 300,000 feet). Their physical composition is also unknown, but they are believed to be composed of fine, cosmic dust particles possibly with a thin, outer layer of ice. Noctilucent clouds become visible after sunset. They are at first greyish, then more brilliant and, as time advances, they appear bluish white like tarnished silver. Other special clouds include clouds from fires produced by the fine combustion products. These may appear as dark, cumulus or cumulonimbus clouds but usually are rapidly dispersed and carried great distances by the wind, spreading to resemble thin, stratiform veils. Clouds from volcanic eruptions, explosions, and industrial activities are also considered in the "special cloud" category.
When the height of a particular cloud is known, the concept of étages may be of some help to the observer in identifying this cloud. Its genus can then be determined by making a choice from among the genera normally encountered in the étage corresponding to its height. Definitions of the various species and varieties is found in the cloud glossary.
Copyright © 1996-2007 Texas A&M University, Texas A&M Meteorology Department and Marion Alcorn.
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