Example of clouds

Some are puffy and sweet, others are gray and uniform while others still are so erratic and capricious that the human mind starts to see things; bunnies, cows or a nation’s borders.The different types of clouds are named based on their shape and how high up they hover in the troposphere. © 2007-2019 ZME Science - Not exactly rocket science.
For instance, the diagram below provides a quick overview of the most common types of clouds based on altitude.A cloud is a visible accumulation of minute droplets of wate, ice crystals, or both, suspended in the air. Clouds may also form in contact with the ground surface, too. All in all, there are ten fundamental types of clouds. The sight of them usually means rainfall is imminent in the next 24 hours.Altocumulus clouds form at a lower altitude so they’re largely made of water droplets though they may retain ice crystals when forming higher up. Though they vary in shape and size, all clouds are basically formed in the same way through the vertical of air above the condensation level. It’s a vertical developing type of cloud whose base grows from one to up to eight kilometers, hence it’s commonly called a tower cloud. However, if enough moisture is retained at the ground level, the cloud can transform into a nimbostratus. Though they vary in shape and size, all clouds are basically formed in the same way through the vertical of air above the condensation level. They resemble cumulus clouds except they’re far bigger. Besides the filament appearance, cirrus clouds stand out among other types of cloud because they’re often colored in bright yellow or red before sunrise and after sunset, respectively. Their color varies from light gray to white and the fibrous bands can vary widely in thickness. When you see a cumulonimbus, you know there’s a thunderstorm waiting to happen somewhere.Cumulonimbus clouds can be seen most commonly during the afternoons of summer and spring months when the Earth’s surface releases heat.Stratocumulus looks like a thick white blanket of stretched out cotton. When altocumulus appears with another cloud type at the same time, storm normally follows. You’ll commonly see this types of clouds in an advancing warm frontal system, preceding nimbostratus clouds.Nimbostratus clouds form as a result of the gradual accumulation of moist area over a large area as the warm frontal system lifts the warm and moist area higher up in the atmosphere where it condenses. Cirrostratus clouds can turn into altostratus clouds if these descend to a lower altitude.As a nice piece of trivia, cirrostratus clouds almost always move in a westerly direction.

You can easily distinguish a stratus cloud by the long horizontal layers of cloud which have a fog-like appearance.The clouds form from large air masses that rise to the atmosphere and later condense. They’re quite translucent which makes it easy for the sun or the moon to peer through. We're here to help make sense of it all:Subscribe now for the news that matter published by professional science journalists.Accurate scientific information is more important than ever. Altocumulus clouds may also form in combination with other types of clouds like cumulonimbus. A cloud is a visible accumulation of minute droplets of wate, ice crystals, or both, suspended in the air. We're here to help make sense of it all:Subscribe now for the news that matter published by professional science journalists. As outlined earlier, a nimbostratus cloud can form from other types of clouds, like a descending altostratus.

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