Cloud Identification - PowerPoint PPT Presentation

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Cloud Identification

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May have been blown off top of cumulonimbus. Cirrus. More Examples of ... mountains, a series of large-scale standing waves may form on the downwind side. ... – PowerPoint PPT presentation

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Title: Cloud Identification


1
Cloud Identification
2
High Clouds
3
Cirrus
  • High
  • Thin, whispy, feather-like
  • Made of ice crystals
  • May have been blown off top of cumulonimbus

4
More Examples of Cirrus Clouds
5
Cirrocumulus
  • High
  • Thin but puffy
  • Often in wave-like patterns
  • Ice
  • Sign of turbulant winds
  • Fast moving

6
More Examples of Cirrocumulus Clouds
7
Middle Altitude Clouds
8
Altocumulus
  • Middle altitudes
  • Puffy, patchy
  • Often in rows to form cloud streets
  • Often occur in advance of a storm

9
More Examples of Altocumulus Clouds
10
  • Middle altitudes
  • Light grey
  • Uniform
  • Covers most of sky
  • Water droplets
  • May indicate changing wind and weather

11
More Examples of Altostratus Clouds
12
Low Altitude Clouds
13
  • Low
  • Puffy, fluffy
  • Looks like cotton balls, cauliflower
  • Fair-weather clouds
  • Flat bottoms

14
More Examples of Cumulus Clouds
15
  • Low
  • Light or dark grey
  • Uniform
  • Covers most of sky
  • Fog is a stratus cloud

16
More Examples of Stratus Clouds
17
  • Low but towering
  • May have anvil shape on top
  • Storm clouds
  • May have thunder, hail, lightening or tornadoes

18
More Examples of Cumulonimbus Clouds
19
Some other Cool Cloud TypesLenticular Clouds
  • Form at high altitudes and are generally aligned
    at right angles to the wind. Where stable moist
    air flows over a mountain or a range of
    mountains, a series of large-scale standing waves
    may form on the downwind side. Lenticular clouds
    sometimes form at the crests of these waves

20
More Lenticular Clouds
21
Still more..incredible!!
22
Wave Clouds
These clouds are formed between two layers of
air, with different densities, traveling at
different speeds. Therefore, if a warm, less
dense layer exists over a layer of colder, denser
air, and the wind shear across the two layers is
strong enough, eddies will develop along the
boundary.
23
Awesome Clouds!!
Go forth and seek clouds!!!!
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