What are the clouds cirrostratus?

Cirrostratus clouds are high -ranked clouds located about 16 404 to 42 650 feet (5,000 to 13,000 meters) above the earth's surface. They take their name from the words cirrus , which means "curled" and stratus , which means "spread". The appearance of Cirrostratus clouds varies between types, but is generally thin and composed of small fibrous Wisps. When you clump together, it is extremely difficult to distinguish one cloud from another. Cirrostratus clouds generally testify to the concentrations of high movement in the upper atmosphere, so their presence is a sign of possible changes in weather.

There are several types of Cirrostratus clouds. Cirrostratus fibibus are clouds that seem like fibrous leaves in the sky. Cirrostratus nebulosus, on the other hand, is much less defined and often resembles fog when they are in groups. Clouds Cirrostratus undulatus have wave patterns, while cirrostratus duplicatus are clouds cirrostratus layered on top of each other. Different types are created based on humidity temperatureand the surrounding area present at the time and location of the creation of clouds. Warm air encounters cold air in the troposphere in even layers. As the humidity cools down in the warm air, it begins to freeze into the ice. The ice, when it is in small sizes and separated in wide spaces, forms clouds cirrostratus. This process also occurs when other types of Cirrus clouds move from one form to another.

The composition and wide gaps of Cirrostratus clouds are very thin, and also translucent. The sun and the moon can be seen more easily through Cirrostratus clouds compared to other types of clouds. The light often bends around and creates a halo across the cloud and creates a halo in the sky. Because these clouds are thin, they are usually indistinguishable apart when they are grouped together.

Cirrostratus clouds have several consequences of weather. Their appearance indicates early accumulation of moisture in the atmosphereera, especially at the top. Although this does not necessarily have to predicate clotting, it is evidenced by the approaching warm queue. If the clouds enter the warm queue, the ice crystals forming a cloud can melt and lead to clotting within one to two days. In the case of Cirrostratus nebulosus, in which ice crystals are at higher temperatures than other types of Cirrostratus clouds, clotting usually occurs within eight to 24 hours.