Clouds Mackenzie Goodwater

Stratus clouds are low-level clouds characterized by horizontal layering with a uniform base, as opposed to convective or cumuliform clouds that are formed by rising thermals. The word "stratus" comes from the Latin prefix "strato-", meaning "layer
A Nimbostratus cloud are dark, low-level clouds accompanied by light to moderately falling precipitation.
Cumulus clouds are puffy clouds that sometimes look like pieces of floating cotton. The base of each cloud is often flat and may be only 3300 feet above the ground.
Altostratus clouds are apart of middle altitude cloud genus belonging to the stratiform physical category characterized by a generally uniform gray to bluish-green and sheet or layer.
Altocumulus clouds are composed primarily of water droplets and are located between 6,500 and 20,000 feet above the ground.
Cumulonimbus clouds are much larger and more vertically developed than fair weather cumulus. They can exist as individual towers or form a line of towers called a squall line. Fueled by vigorous convective updrafts, the tops of cumulonimbus clouds can easily reach 39,000 feet or higher.
Cirrocumulus clouds are small rounded puffs that usually appear in long rows high in the sky. Cirrocumulus are usually white, but sometimes appear gray.
The most common form of high-level clouds are thin and often wispy cirrus clouds. Typically found at heights greater than 20,000 feet, cirrus clouds are composed of ice crystals that originate from the freezing of supercooled water droplets. Cirrus generally occur in fair weather and point in the direction of air movement at their elevation.

Credits:

Created with images by AdinaVoicu - "sun sunset sky" • Brandon Morse - "cloud" • FrankWinkler - "coast elgol isle of skye" • redamokhtar - "sky birds cloud" • Photodesaster - "Clouds" • Hans - "cloud afterglow red" • LoggaWiggler - "sunset abendstimmung lake" • pruzi - "lake evening sunset" • zimpenfish - "Clouds"

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