Shocking, the cloud is a sword = Mengejutkan, awan berbentuk pedang

In meteorology, a cloud is an aerosolcomprising a visible mass of minuteliquid droplets, frozen crystals, or particles suspended in theatmosphere above the surface of aplanetary body.^[1] The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, andmesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch ofmeteorology.

There are two methods of naming clouds in their respective layers of the atmosphere; Latin and common. Cloud types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names due to the universal adaptation of Luke Howard'snomenclature. Formally proposed in 1802, it became the basis of a modern international system that divides clouds into five physical forms that appear in any or all of three altitudelevels (formerly known as étages). These physical types, in approximate ascending order of convective activity, include stratiform sheets, cirriformwisps and patches, stratocumuliformlayers (mainly structured as rolls, ripples, and patches), cumuliformheaps, and very large cumulonimbiformheaps that often show complex structure. The physical forms are divided by altitude level into ten basic genus-types. The Latin names for applicable high-level genera carry acirro- prefix, and an alto- prefix is added to the names of the mid-level genus-types. Most of the genera can be subdivided into species and further subdivided into varieties.