Lenticular clouds can be described as stationary clouds that are usually formed within the troposphere. This type of cloud tends to be perpendicularly aligned with the direction of the blowing wind (Ahrens & Henson, 2015). The main types of lenticular clods are the stratocumulus standing lenticular, the altocumulus standing lenticular, and the cirrocumulus standing lenticular. The process of lenticular cloud formation involves the obstruction of air travel by natural features and artificial structures. The disruption will lead to the formation of eddies current which causes significant turbulence. The movement of stable and moist air over the resulting eddies will lead to condensation and the formation of lenticular clouds. The clouds have a saucer or lens appearance that makes them unique. Since the lenticular clouds are largely unique, they have also been considered to be an explanation for unidentified flying object sightings. The second type of cloud is the cumulus which has flat bases and a fluffy appearance. These low-level clouds appear in clusters and lines. Furthermore, they are usually considered to be the precursor of various types of clouds depending on weather factors such as temperature, moisture level, and instability. The cloud is less than 2000m meters from the sea level except in the case of the vertically oriented type (Ahrens, 2006). It is imperative to state that the cumulus clouds produce minimal precipitation. They are formed when water vapor is supercooled as a result of temperature changes. The appearance of the cumulus clouds may differ based on the ambient temperature (Ahrens, 2006). This can be an indication of incoming solar radiation, a free-convective environment, or limited convection. In some instances, the cumulus clouds can grow upwards. An example is a case where they develop to form giant cumulonimbus clouds that are linked to thunderstorms. Therefore, the appearance and environmental significance of the cumulus clouds may differ depending on the prevailing conditions in an area.
References
Ahrens, D., & Henson, R. (2015). Meteorology today . Cengage Learning.
Ahrens, D. (2006). Meteorology today . Cengage Learning.
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