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The symbol for a rainy day on a weather map is usually a cloud with raindrops falling from it. It indicates that there is precipitation occurring in the form of rain in that area.
The noun 'raindrops' is the plural form of the singular noun 'raindrop'; a common, compound, concrete noun; a word for a unit of water falling from a cloud; a word for a thing.
precipitation
Dj Raindrops
The primary difference between a cloud droplet and a raindrop is their size. Cloud droplets are much smaller, typically less than 0.02 mm in diameter, while raindrops are larger and can range from 0.5 to 6 mm in diameter. Cloud droplets need to grow through collision and coalescence to form raindrops and eventually fall to the ground as rain.
Cloud drops are tiny water droplets that form in clouds and are too small to fall to the ground, while raindrops are larger droplets that have grown in size and weight enough to fall as precipitation. Cloud drops are typically less than 0.02 inches in diameter, while raindrops can range from 0.02 to 0.2 inches in diameter.
Hail forms when updrafts in thunderstorms carry raindrops into colder regions of the atmosphere. As the raindrops freeze, they grow in size and eventually fall to the ground as hailstones. Hail is typically associated with cumulonimbus clouds, which are large, towering clouds that produce thunderstorms.
Let's estimate. If the storm creates .2 inches of rain fall over a 10 square mile area, then the volume is 10 x 5280 x 5280 x 12 x 12 x 0.2 x (2.543) = 131571396005.0688 cm3 of rainwater. Assuming that each cm3 is the equivalent of 20 rain drops, then there are 2631427920101.376 raindrops. Since this is an estimate, let's round to 2630,000,000,000 raindrops.
Gaseous
Raindrops can vary in size, but on average they are about 1 to 2 millimeters in diameter. Some larger raindrops may be 4 to 6 millimeters in diameter, while smaller raindrops can be less than 1 millimeter in diameter.
No, warm clouds typically form raindrops by the collision-coalescence process where cloud droplets collide and merge together to form larger droplets. The Bergeron process is usually associated with the formation of precipitation in cold clouds where ice crystals grow at the expense of liquid droplets.
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