Stratus Clouds—a Veil of Gray

Stratus clouds

Stratus clouds are uninteresting, flat, heavy horizontal clouds that lay low within the sky. They’re often grey however may also be white.

Stratus clouds continuously carry a drizzle or they are able to carry snow.

The altitude of stratus clouds point out how briskly a hurricane is drawing near. Low stratus clouds generally imply rain will start quickly.

Stratus clouds seem as a hazy veil. They’re featureless and miserable. Every so often they’re known as “high fog.” They at all times difficult to understand the solar.

The phrase “stratus” comes from the Latin prefix “strato-“, meaning “layer”.

Stratus clouds shape when a uniform sheet of quite heat, wet air rises up and involves leisure in opposition to a better, uniform sheet of heavier cool air. Stratus clouds point out that the ambience is arranged into solid horizontal layers. This often occurs when a entrance of heat air is advancing in opposition to a mass of chilly air.

Altostratus clouds

Stratus clouds continuously linger for days as extended cloudy climate.

When a stratus cloud produces precipitation it is named a nimbostratus cloud. Darkish, heavy nimbostratus clouds can drop stable rain for hours.

Heavy, horizontal stratus clouds may also be contrasted to cumulus clouds which can be shaped by means of accumulations of heat air emerging in columns.

When an accumulation of heat air breaks thru a better mass of cool air it might probably billow as much as shape a stratocumulus cloud.  When stratus clouds shape upper than 7,000 ft, they’re known as altostratus clouds.

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