Types of Clouds

736 Words2 Pages

Like low level clouds, the most basic classification of middle clouds also based on their elevation from earth’s surface. Middle level clouds exist between 2 km to 6 km above of the surface. Middle level clouds were classified into 3 types which is Altocumulus, Altostratus and Nimbostratus (Oliver, 2005). All of these clouds are occur in layers but it different in colour, precipitation and description of the clouds. Altocumulus can be found word widely at middle latitude. It consists of water and ice of crystal. Altocumulus is relatively thin and has different in clouds element such as distinct form because of the several species and types of altocumulus that been identify. It also may exist in different elements like long rolls, tuft of wools (Altocumulus floccus) and castle shaped (castellanus). For precipitation, altocumulus may produce light shower. Altocumulus occurs in white or grey in colours and sometimes it will forms both white and grey of patch, sheet or layers generally with shading, consist of laminae, patch and etc. (Hauze, 1993). Altostratus has fibrous or uniform appearance compare to altocumulus. These world-wide clouds consist of water and crystal of ice. Its covering the sky totally and sun can reveal at least vaguely as through ground glass because altostratus having parts thin (Hauze, 1993). Altostratus can be seen clearly at the top of mountains. Sometimes corona which is the light of sun and moon can be seen in the altostratus. In Altostratus clouds, rain and snow usually form and bring storms at the same times. Even it covers the whole skies and appear in grey-blue colour, the sunlight still may go trough but transform into water or fuzzy. For altostratus precipitation, it is prolonged but in light rain or... ... middle of paper ... ...Cirrostratus. Cirrostratus clouds difficult to see because it appear in the form of lightning spot in the sky. Differ from other clouds, cirrostratus did not block the sun rays but when we see in the skies its look like the combination of clouds and rays. Cirrostratus consists of ice crystal and also produces halo phenomenon. It looks very nice when we see from the bottom view. Cirrostratus formed when cirrus clouds are joining and spreading. For cirrostratus clouds, it has none precipitations. Cirrostratus is transparent clouds, smooth appearance and white in colour and totally covered skies (Hauze, 1993). Works Cited Houze, R. A. (1993). Cloud dynamics. San Diego: Academic Press. Oliver, J. E. (2005). Encyclopedia of world climatology. Dordrecht, Netherlands: Springer. Pinney, G. (2011). The cloud collector's handbook. San Francisco, Calif.: Chronicle Books.

Open Document