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Clouds
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Cloud formation Large mass of air rises, cools to dew point
Condensation (or deposition) occurs on condensation nuclei salt, dust, soil, pollutants
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elevation at which air becomes saturated is lifting condensation level (flat base of clouds)
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A cloud is a mass of suspended water, supercooled water and/or ice particles.
particles micrometers Water is supercooled : liquid below freezing
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< -40oC (-40°F): all ice crystals
< -20oC: predominantly ice crystals -12o to -20o C: mixture of ice and supercooled water > -12oC (10°F): all water
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Cloud classification (according to shape and altitude)
Shape Classes: Flat: stratiform Globular: cumuliform
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Altitude Families: High Cloud (cirro-): ice crystal clouds
> 6000 m (20,000 ft.) CIRRUS, CIRROSTRATUS, CIRROCUMULUS
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cirrus
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cirrus
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Cirrostratus (halo around sun or moon)
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cirrostratus
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cirrocumulus
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Altitude Classes: Middle Cloud (alto-)
3000 – 6000 m (10, ,000 ft.) ALTOSTRATUS, ALTOCUMULUS
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altostratus
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altostratus
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altostratus
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altocumulus
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altocumulus
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altocumulus
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altocumulus
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Altitude Classes: Low Cloud (stratus) <3000 m (10,000 ft)
STRATUS, NIMBOSTRATUS, STRATOCUMULUS
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stratus
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stratus
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stratus
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nimbostratus
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stratocumulus
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stratocumulus
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stratocumulus
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Altitude Classes: Vertically developed clouds (CUMULONIMBUS)
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Vertically Developed Clouds: cumulonimbus
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cumulonimbus
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cumulonimbus
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cumulonimbus
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mammatus
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lenticular Strong wind flow over rugged terrain often stacked
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Cumulonimbus pileus
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Cumulus fractus (small, ragged)
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Cumulus humilis (smaller vertical extent)
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Altocumulus translucidus
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Altostratus translucidus
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Altocumulus undulatus
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contrails
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contrails
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