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Lenticular clouds, technically known as altocumulus standing lenticularis, are stationary lens-shaped clouds that form at high altitudes, normally aligned at right-angles to the wind direction. Where stable moist air flows over a mountain or a range of mountains, a series of large-scale standing waves may form on the downwind side. Lenticular clouds sometimes form at the crests of these waves. Under certain conditions, long strings of lenticular clouds can form, creating a formation known as a wave cloud.
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Lens-shaped clouds are called lenticular clouds. They are formed when moist air flows over a mountain or obstacle and creates standing waves in the atmosphere, causing the air to cool and condense into these distinctive cloud formations.
The process in which clouds are formed in the water cycle is called condensation. This occurs when warm, moist air rises, cools, and condenses into tiny water droplets or ice crystals that gather to form clouds.
Lens-shaped clouds, also known as altocumulus lenticularis clouds, are formed at high altitudes by strong winds flowing over mountains or other obstructions. The air is forced to rise and cool, condensing into cloud droplets. The resulting clouds can appear smooth and lens-like, often stacked in a row perpendicular to the wind direction.
That is called rain. Rain is formed when water droplets in clouds combine to create larger droplets that fall to the ground due to gravity.
Positive charges in clouds are called protons, while negative charges are called electrons. When these charges become separated within a cloud, it can lead to the formation of lightning.
Mares' tails are a type of cloud called cirrus clouds. Cirrus clouds are wispy, high-altitude clouds formed by ice crystals and typically appear as thin, feathery strands. They are often seen as a sign of approaching changes in weather.