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Cloud | A Wisdom Archive on Cloud |  | Cloud A selection of articles related to Cloud |  |
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More material related to Cloud can be found here:
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cloud, Cloud, Cloud - Cloud classification, Cloud - Cloud formation and properties, Cloud - Clouds on other planets, Cloud - Colors of clouds, Cloud - Global dimming, Cloud - High clouds Family A, Cloud - Hot Ice and Ice Memory in cloud formation, Cloud - Low clouds Family C, Cloud - Middle clouds Family B, Cloud - Other clouds, Cloud - Vertical clouds Family D, Cloud albedo, Cloud feedback, Cloud base, Cloud forcing, Cloud types, Fog, Mushroom cloud, Precipitation, Coalescence, Tornado, Hurricane, Monsoon, Thunderstorm, Weather lore, Mammatus, Extraterrestrial skies
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ARTICLES RELATED TO Cloud | |
 |  |  | Cloud: Encyclopedia II - Cloud - Cloud classification
Clouds are divided into two general categories: layered and convective. These are named stratus clouds (or stratiform, the Latin stratus means layer) and cumulus clouds (or cumiloform, cumulus means piled up). These two cloud types are divided into four more groups that distinguish the cloud's altitude. Clouds are classified by the cloud base height, not the cloud top. This system was proposed by Luke Howard in 1802 in a presentation to the Askesian Society.
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See also:Cloud, Cloud - Cloud formation and properties, Cloud - Hot Ice and Ice Memory in cloud formation, Cloud - Cloud classification, Cloud - High clouds Family A, Cloud - Middle clouds Family B, Cloud - Low clouds Family C, Cloud - Vertical clouds Family D, Cloud - Other clouds, Cloud - Colors of clouds, Cloud - Global dimming, Cloud - Clouds on other planets Read more here: » Cloud: Encyclopedia II - Cloud - Cloud classification |
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 |  |  | Cloud: Encyclopedia II - Cloud - Cloud classificationClouds are divided into two general categories: layered and convective. These are named stratus clouds (or stratiform, the Latin stratus means layer) and cumulus clouds (or cumuliform, cumulus means piled up). These two cloud types are divided into four more groups that distinguish the cloud's altitude. Clouds are classified by the cloud base height, not the cloud top. This system was proposed by Luke Howard in 1802 in a presentation to the Askesian Society.
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See also:Cloud, Cloud - Cloud formation and properties, Cloud - Hot Ice and Ice Memory in cloud formation, Cloud - Cloud classification, Cloud - High clouds Family A, Cloud - Middle clouds Family B, Cloud - Low clouds Family C, Cloud - Vertical clouds Family D, Cloud - Other clouds, Cloud - Colors of clouds, Cloud - Global dimming, Cloud - Clouds on other planets Read more here: » Cloud: Encyclopedia II - Cloud - Cloud classification |
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 |  |  | Cloud: Encyclopedia II - Cloud - Cloud formation and propertiesClouds form when the invisible water vapor in the air condenses into visible water droplets or ice crystals. This can happen in two ways.
http://www.ems.psu.edu/~fraser/Bad/BadClouds.html
1. The air is cooled below its saturation point. This happens when the air comes in contact with a cold surface or a surface that is cooling by radiation, or the air is cooled by adiabatic expansion (rising). This can happen
along warm and cold fronts (frontal lift),
where air flows up the side of a mountain and cools as ...
See also:Cloud, Cloud - Cloud formation and properties, Cloud - Hot Ice and Ice Memory in cloud formation, Cloud - Cloud classification, Cloud - High clouds Family A, Cloud - Middle clouds Family B, Cloud - Low clouds Family C, Cloud - Vertical clouds Family D, Cloud - Other clouds, Cloud - Colors of clouds, Cloud - Global dimming, Cloud - Clouds on other planets Read more here: » Cloud: Encyclopedia II - Cloud - Cloud formation and properties |
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 |  |  | Cloud: Encyclopedia II - Cloud - Cloud formation and propertiesClouds form when the invisible water vapor in the air condenses into visible water droplets or ice crystals. This can happen in three ways.
1. The air is cooled below its saturation point. This happens when the air comes in contact with a cold surface or a surface that is cooling by radiation, or the air is cooled by adiabatic expansion (rising). This can happen
along warm and cold fronts (frontal lift),
where air flows up the side of a mountain and cools as it rises higher into the atmosphere (orographic lift),< ...
See also:Cloud, Cloud - Cloud formation and properties, Cloud - Hot Ice and Ice Memory in cloud formation, Cloud - Cloud classification, Cloud - High clouds Family A, Cloud - Middle clouds Family B, Cloud - Low clouds Family C, Cloud - Vertical clouds Family D, Cloud - Other clouds, Cloud - Colors of clouds, Cloud - Global dimming, Cloud - Clouds on other planets Read more here: » Cloud: Encyclopedia II - Cloud - Cloud formation and properties |
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