When they appear, a storm usually precedes. They often appear next to cirrus clouds and indicate that the weather will change in about twelve hours. When the sky appears covered with this type of clouds, it is said to be boring.
The clouds are totally white without presenting any shadow. These clouds form an almost continuous layer that has a wrinkled surface appearance and with rounded shapes as if they were small cotton flakes. Types of clouds and their characteristics: Cirrocumulus Usually, a sharp decrease in temperatures. If the entire sky is covered with cirrus clouds, it is very likely that a sharp change in weather will occur in 24 hours. It appears as if the sky had been painted with brush strokes. It can be seen with the naked eye looking at the sky. They are like long, thin filaments that have a more or less regular distribution in the form of parallel lines. These clouds are nothing more than clouds formed by ice crystals due to the altitude at which they are found. They are also known as “horse tail” clouds. These are white clouds, transparent and without internal shadows. Types of clouds and their characteristics: Cirrus We are listing the different types of clouds based on the altitude at which they form. Usually the latter are the cause of rains and storms. On the other hand, those that are formed between winds or air with strong vertical currents present a great vertical development.
Clouds that are created when the air is at rest tend to appear in layers or strata. If the temperature is too low, the cloud that forms will be made up of ice crystals.Īnother factor that affects cloud formation is air movement. There are also some types of clouds that give precipitation and others that do not.
The lower the formation temperature, the “thicker” the cloud will be. There are some clouds that form at higher temperatures and some lower ones. Why are they different types of clouds?ĭifferences between cloud formations are due to condensation temperatures. The particles are so small that they are able to be held in the air by slight vertical currents. This water vapor is invisible to the naked eye, as it is made up of water droplets and ice particles. When it reaches a cooler layer of air, it condenses into water vapor. As you ascend in altitude, the environmental thermal gradient causes the temperatures to be lower. High-temperature air becomes less dense, so it tends to rise and be replaced by colder, denser air. When the sun’s rays heat the Earth’s surface, they also heat the surrounding air. For there to be clouds in the sky, there must be a cooling of the air. Before we begin to describe the types of clouds we have to explain how they form.
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