Weather Ch. 16.

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Presentation transcript:

Weather Ch. 16

Clouds Clouds form as warm air is forced upward, expands, and cools As the air cools, the amount of water vapor needed for saturation decreases and the relative humidity increases

Clouds When the relative humidity reaches 100%, the air is saturated Water vapor begins to condense in tiny droplets around small particles such as dust and salt Billions of these droplets form a cloud

Classifying Clouds Classified mainly by shape and height Large amount of variety

Cloud Types Stratus—form layers or smooth sheets in the sky

Cloud Types Cumulus—masses of puffy, white clouds

Cloud Types Cirrus—high, thin, white, feathery clouds

Cloud Height Cirro- = high clouds Alto- = middle-elevation clouds Strato- = low elevations Some cloud names combine the altitude prefix with the term stratus or cumulus

Rain and Snow Clouds Clouds associated with rain or snow often have the word nimbus attached to them Nimbus = dark rain cloud Cumulonimbus Nimbostratus