Title: Cloud Identification
1Cloud Identification
2High Clouds
3Cirrus
- High
- Thin, whispy, feather-like
- Made of ice crystals
- May have been blown off top of cumulonimbus
4More Examples of Cirrus Clouds
5Cirrocumulus
- High
- Thin but puffy
- Often in wave-like patterns
- Ice
- Sign of turbulant winds
- Fast moving
6More Examples of Cirrocumulus Clouds
7Middle Altitude Clouds
8Altocumulus
- Middle altitudes
- Puffy, patchy
- Often in rows to form cloud streets
- Often occur in advance of a storm
9More Examples of Altocumulus Clouds
10- Middle altitudes
- Light grey
- Uniform
- Covers most of sky
- Water droplets
- May indicate changing wind and weather
11More Examples of Altostratus Clouds
12Low Altitude Clouds
13- Low
- Puffy, fluffy
- Looks like cotton balls, cauliflower
- Fair-weather clouds
- Flat bottoms
14More Examples of Cumulus Clouds
15- Low
- Light or dark grey
- Uniform
- Covers most of sky
- Fog is a stratus cloud
16More Examples of Stratus Clouds
17- Low but towering
- May have anvil shape on top
- Storm clouds
- May have thunder, hail, lightening or tornadoes
18More Examples of Cumulonimbus Clouds
19Some 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
20More Lenticular Clouds
21Still more..incredible!!
22Wave 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.
23Awesome Clouds!!
Go forth and seek clouds!!!!