1 How can clouds form? • Air needs to be cooled to saturation. I.e. air cooled to dew point. I.e air reaches 100% RH 1) As air rises, it cools * How to force air to rise: – Topography – fronts – convection – Convergence ---> <---- 2) Surface cools off quickly by emitting radiation 3) Air moves over colder surface/ into cooler area
How can clouds form?. Air needs to be cooled to saturation. I.e. air cooled to dew point. I.e air reaches 100% RH As air rises, it cools * How to force air to rise: Topography fronts convection Convergence --->
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Transcript
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How can clouds form?
• Air needs to be cooled to saturation. I.e. air cooled to dew point. I.e air reaches 100% RH
1) As air rises, it cools* How to force air to rise:
2) Surface cools off quickly by emitting radiation
3) Air moves over colder surface/ into cooler area
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Cloud characteristicsCloud characteristics• Clouds are identified by their height (low, medium
and high) and by their visual characteristics (flat or puffy).
• The four basic cloud groups are:– Cirrus: _________________________– Cumulus: _______________________– Stratus: ________________________– Nimbus: ________________________
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Where do these terms come from?
• The basic classification terminology has Latin roots:– Stratus (Latin for "layer") to describe sheet-like (stable)
clouds. – Cumulus (Latin for "puffy") to denote a cloud with
some puffy vertical (unstable) extent. – Cirrus (Latin for "curl of hair") denotes a wispy high
level cloud.– Nimbus (Latin for "violent rain") means a rain cloud.
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Cloud ClassificationCloud ClassificationAs a first distinction, we classify As a first distinction, we classify
clouds by the height of the clouds by the height of the cloud basecloud base..
LOW CLOUDSLOW CLOUDS
• Low clouds have a base Low clouds have a base below 5000ft.below 5000ft.
• Stratocumulus (Sc), Stratocumulus (Sc), Stratus (St) and are the Stratus (St) and are the primary low-level cloudsprimary low-level clouds
• High clouds typically refer High clouds typically refer to clouds with a base to clouds with a base above 7 km (23,000ft) above 7 km (23,000ft) altitude.altitude.
• Cirrus (Ci), Cirrostratus Cirrus (Ci), Cirrostratus (Cs), and Cirrocumulus (Cs), and Cirrocumulus (Cc) are all high level (Cc) are all high level clouds.clouds.
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Cloud ClassificationCloud Classification
• High level clouds tend to be High level clouds tend to be fuzzy in comparison to low fuzzy in comparison to low level clouds.level clouds.
• This is primarily because This is primarily because high level clouds are made high level clouds are made of ice crystals instead of of ice crystals instead of droplets.droplets.
• Ice crystals usually Ice crystals usually evaporate slowly and thus evaporate slowly and thus have more time to diffuse.have more time to diffuse.
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Cloud ClassificationCloud ClassificationThree primary cloud classes overlap the height bands:Three primary cloud classes overlap the height bands:
– Cumulus (Cu)Cumulus (Cu)
– Cumulonimbus (Cb)Cumulonimbus (Cb)
– Nimbostratus (Ns)Nimbostratus (Ns)
““nimb-”nimb-” defines that the cloud is precipitating. defines that the cloud is precipitating.
““cumul-”cumul-” defines that the clouds are a result of convection. defines that the clouds are a result of convection.
““strat-”strat-” defines that the clouds are layered clouds. defines that the clouds are layered clouds.
Various terms are commonly intermixed and aren’t limited Various terms are commonly intermixed and aren’t limited to any given altitude. to any given altitude.