cloud - soest · cloud classification clouds are categorized by their (cloud base) height,...

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1 Cloud Formation All clouds require 3 things 1. Water vapor 2. Cloud Condensation nuclei (CCN) 3. Cooling - heat transfer out of air parcel or work done by air molecules in parcel. (1) Lifting – most clouds form when air is lifted. a) Convergence – low press center – stratus b) Mountains – lifting by terrain c) Fronts – lifting over denser air. d) Warm air relative to surroundings i) Fires, volcanoes – cumulus ii) Latent heat (2) Mixing – seeing your breath on cold day (3) Contact – with cold surface: advection fog (4) Radiation – fog in winter mornings Mechanisms for Cooling the Air

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Page 1: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Cloud FormationAll clouds require 3 things

1. Water vapor2. Cloud Condensation nuclei (CCN)3. Cooling - heat transfer out of air parcel

or work done by air molecules in parcel.

(1) Lifting – most clouds form when air is lifted.a) Convergence – low press center – stratusb) Mountains – lifting by terrainc) Fronts – lifting over denser air.d) Warm air relative to surroundings

i) Fires, volcanoes – cumulusii) Latent heat

(2) Mixing – seeing your breath on cold day

(3) Contact – with cold surface: advection fog

(4) Radiation – fog in winter mornings

Mechanisms for Cooling the Air

Page 2: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Cloud classificationClouds are categorized by their (cloud base) height, appearance, and vertical development– High Clouds - generally above 16,000 ft (>5 km) at

middle latitudes and up to the tropopause• Main types - Cirrus, Cirrostratus, Cirrocumulus

– Middle Clouds – 7,000-23,000 feet (2-7 km)• Main types – Altostratus, Altocumulus

– Low Clouds - below 6,500 ft (2 km)• Main types – Stratus, stratocumulus,

nimbostratus– Vertically developed clouds (via convection)

• Main types – Cumulus, Cumulonimbus

Cellular structure in a top viewRayleigh-Benard convection

Cellular structure of stratocumulus clouds over the NE Pacific (9/14/06)

10o

Page 3: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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High Clouds• White in day; read/orange/yellow at

sunrise/sunset• Made of ice crystals

Cirrus (Ci)• Thin and wispy• Move toward the east• Indicate fair weather

Cirrocumulus (Cc)• Less common than crirrus• Small, rounded white puffs individually

or in long rows (fish scales; mackerel sky)

Cirrostratus (Cs)• Thin and sheet-like• Sun/moon clearly visible through them• Halo common• Often precede precipitation

Cirrus

High Clouds• White in day; read/orange/yellow at

sunrise/sunset• Made of ice crystals

Cirrus (Ci)• Thin and wispy• Move toward the east• Indicate fair weather

Cirrocumulus (Cc)• Less common than crirrus• Small, rounded white puffs individually

or in long rows (fish scales; mackerel sky)

Cirrostratus (Cs)• Thin and sheet-like• Sun/moon clearly visible through them• Halo common• Often precede precipitation

Cirrocumulus

Page 4: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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High Clouds• White in day; read/orange/yellow at

sunrise/sunset• Made of ice crystals

Cirrus (Ci)• Thin and wispy• Move toward the east• Indicate fair weather

Cirrocumulus (Cc)• Less common than crirrus• Small, rounded white puffs individually

or in long rows (fish scales; mackerel sky)

Cirrostratus (Cs)• Thin and sheet-like• Sun/moon clearly visible through them• Halo common• Often precede precipitation

Cirrostratus

Middle Clouds• Altostratus (As)

– Gray, blue-gray– Often covers entire sky– No halo– Sun or moon may show

through dimly• Usually no shadows

• Altocumulus– <1 km thick– mostly water drops– Gray, puffy– Differences from cirrocumulus

• Larger puffs• More dark/light contrast

Altostratus (As)

Page 5: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Middle Clouds• Altostratus

– Gray, blue-gray– Often covers entire sky– Sun or moon may show

through dimly• Usually no shadows

• Altocumulus (Ac)– <1 km thick– mostly water drops– Gray, puffy– Differences from cirrocumulus

• Larger puffs• More dark/light contrast

Altocumulus (Ac)

Low CloudsStratus (St)• Uniform, gray• Resembles fog that does not reach the ground• Usually no precipitation, but light mist/drizzle possible

Page 6: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Stratocumulus (Sc)• Low lumpy clouds• Breaks (usually) between cloud elements• Lower base and larger elements than altostratus

Low Clouds

Nimbostratus (Ns)• Dark gray• Continuous light to moderate rain or snow• Evaporating rain below can form fractus

Low Clouds

Page 7: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Cumulus (Cu)• Puffy “cotton”• Flat base, rounded top• More space between cloud elements than stratocumulus

Vertically Developed Clouds

Cumulus Congestus• Towering cumulus• Rain showers

Vertically Developed Clouds

Page 8: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Cumulonimbus (Cb)• Thunderstorm cloud• Very tall, often reaching tropopause, often with anvils• Individual or grouped• Violent vertical motion that may exceed 50 knots• Large energy release from water vapor condensation

Vertically Developed Clouds

Page 9: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Cloud type (Fog is just one type of cloud that touches ground)

Page 10: cloud - SOEST · Cloud classification Clouds are categorized by their (cloud base) height, appearance, and vertical development – High Clouds - generally above 16,000 ft (>5 km)

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Stc

Cb

Cu

Cu

Visible

Cb Ci

Cu

Infrared