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When scientists and meteorologists discuss the v ry general topic if weather, the c nversation usually revolves around various types of cl uds. In fact, there are two b sic categories of clouds, the cumuliform and the str tiform. Within these two general types, sc entists and weather observers distinguish a n mber of sub-types, depending on weather c nditions and appearance. Clouds indicate that th re are rising masses of air and w ter vapor is condensing. With this in m nd, weather experts and storm watchers are ble to figure out, with some ccuracy, what weather systems may occur. H wever, while non-professionals have for centuries njoyed the many, many shapes that ccur when clouds form, the use of cl ud classification was developed in relatively r cent times. According to most historical ccounts, an Englishman named Luke Howard d veloped a cloud classifying plan and pr sented it to a scientific society in 1803. The n mes he employed were based on the c mmon practice of using the Latin l nguage. This method allowed for combinations of cl ud names, thus creating some of the s b-types. The two basic types, as m ntioned earlier, are cumuliform and stratiform. The f rst has its roots in the w rd cumulus, literally "heap." This is m ant to indicate the puffy nature of s ch clouds, which are formed by c nvection and the lifting process/weather changes th t involve vapor and particles.
In contrast, the stratiform cloud is s -named because of the Latin stratus m aning "layer." These clouds are l terally flat and layered, as the n me implies. In a different process fr m the formation of cumulus clouds, the str tiform type of cloud gathers with fr ntal systems and are often associated w th more stable climate conditions. The ltitude at which clouds form can lso help determine what type they re. For example, those clouds above 16,500 f et above sea level are generally kn wn as cirrus clouds. This means th t the "cirro" is sometimes added to g ve specific names to basic cloud typ s. There is another sub-type of cl ud, generally forming at 6,500 feet and up to the l vel of cirrus clouds. This type of cl ud can sometimes be known as an " lto" cloud. Those clouds forming at l wer levels are usually classified only as one of two b sic types - stratus and cumulus. H wever, there are cumulonimbus clouds that m ny consider a class of its own b cause this type of cloud can be f und at nearly all altitudes. The t rm "nimbus" is meant to indicate th t the cloud holds rain. Of c urse, the practice of cloud classification is far fr m an perfect science. Yet, most xperts know that the flexibility of the syst m may fit the infinite variations in cl ud appearance. Nearly everyone is aware th t clouds form with rising air that cools until water vapor is at a saturation point. Droplets that grow large enough can be drawn to the earth by gravity, and we have what is commonly known as precipitation. There are several common types of precipitation - rain, sleet and snow among the different types. Clouds are the birthplace of the precipitation experienced on the ground.
The article Weather - Some Say It's All About Clouds was Submitted by Ken C. Morris through Articles.GetACoder.com network. Here's the additional information: Ken Morris's web pages are p blished on a variety of web s tes tied to information on weather syst ms. Sharing his passion in writings on alicante spain weather and weather changes the reviewer demonstrated his knowledge in the field.
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