Classifying Clouds Is An Important Part Of Weather Study

From technical analysis we conclude that rising airof clouds, height prefixes can be combined with
masses and condensing air vapor manifestbasic types. Thus layer clouds at mid-level
themselves through clouds. By observing the cloudaltitudes are termed allostratus clouds.
shapes weather forecasters can feel the presentSince too familiar cumulonimbus cloud extends
and upcoming weather events. From the aestheticfrom low to high altitudes it itself is taken as a
point of view, the endless variety of beautifulcategory. It is bears rain and the word nimbus
clouds has remained a source of immense delightmeans just that.
for mankind from the very beginning.Not really a science classification of clouds is. Still
Interestingly, until the early 19th century noconsidering the fact that clouds vary all the time
system was developed for classification of clouds.and the variations are of endless forms, the best
An English scientist, Luke Howard, presented aresults can be obtained through a classification
classification scheme to his local scientific societysystem that is flexible.
in 1803. Howard classified the basic cloud shapesWhat does precipitation mean?
and the language he used was Latin, the languageWhen air rises and cools till it is saturated with
of science. Since combination of words waswater vapor clouds formation takes place. In such
allowed in his system that left the scope fora condition, water vapor condenses into tiny
further classification. Immediate acceptance andwater droplets or sublimates into tiny crystals of
universal admiration were the gains of his system.ice. However due to gravity tiny water droplets
In our time cumuliform and stratiform are theor ice crystals fall into the ground if they become
two basic types of classification to start with.quite b big. Precipitation signifies this fall.
From cumulus, the Latin equivalent of heap, theDetermination of how it should be classified
word cumuliform is derived. Puffy clouds are calleddepends on the form in which the precipitation
cumiliform clouds. From convection or orographicreaches the ground. On the process of formation,
lifting this type is generated normally.temperatures within and below the cloud and the
From stratus, the Latin equivalent of layer, theground temperatures as well depends whether
word stratiform is derived. A flat, layered shape isprecipitation will fall as rain, freezing rain, sleet, or
the characteristic of straiform clouds. Normallysnow.
with the accompaniment of stable weatherDepending on water droplet size and quantity,
appear stratiform clouds.steady or intermittent can be the classification of
Further classification of these two basic types isthe precipitation. Steady or intermittent can also
possible if the heights at which they form arebe the classification of the precipitation. Normally
taken into consideration. The term cirrus cloudswith frontal activity steady precipitation is
are applied to high-level clouds beyond 16,500associated, and with convection and atmospheric
feet. To a basic cloud type the prefix cirro isinstability is the association of intermittent
sometimes added. For clouds developed in theprecipitation.
range of 6,500 to 16,500 feet the pr4ix alto isNext time you visit Spain you can use all this
applied. No prefix is applicable for clouds developedknowledge to judge if the time is right to visit all
below 6,500 feet and therefore the basic types,the places in Malaga or if it is better to stay in
stratus and cumulus, are denoted by default asyour hotel room and enjoy the rain from the
low-level clouds. For signifying quite a few typeswindow.