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Lecture 9 (11/04) METR 1111

Lecture 9 (11/04) METR 1111. Cloud Types. Cloud Classification. In 1803, Luke Howard devised the basic system of cloud classification Still used today Based on Latin names Two parts to a cloud’s name: - Shape (ex: cirrus, stratus, cumulus) - Height (cloud base & vertical extent).

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Lecture 9 (11/04) METR 1111

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  1. Lecture 9 (11/04)METR 1111 Cloud Types

  2. Cloud Classification • In 1803, Luke Howard devised the basic system of cloud classification • Still used today • Based on Latin names • Two parts to a cloud’s name: - Shape (ex: cirrus, stratus, cumulus) - Height (cloud base & vertical extent)

  3. Shapes & Heights • Shapes - Cirrus = curly and wispy - Stratus = layered or stratified - Cumulus = lumpy or piled up • Heights - Cirro = high (bases above 20,000 ft) - Alto = mid level (bases 7,000-20,000 ft) - Nimbo = producing precipitation

  4. What do clouds tell us? • Clouds just don’t happen - there’s always a reason • A particular cloud’s shape and location depend on (and can therefore tell us about): - the movement of the air - amount of water vapor in air - stability (flat clouds = stable air while puffy clouds = unstable air)

  5. Cirrus Clouds • Cirrus = high altitude wispy clouds • Quite thin and often have a hairlike or filament type of appearance. • Made up of ice particles • The curled up ends (called mares’ tales) as depicted in the following picture are very common features.

  6. Cirrus Photo

  7. Stratus Clouds • Stratus clouds are usually the lowest of the low clouds. • Often appear as an overcast deck (as shown in next slide), but can be scattered. • The individual cloud elements have very ill-defined edges compared to cumulus • Fog is just stratus clouds on the surface

  8. Stratus Photo

  9. Fog (Stratus on Ground) Photo

  10. Cumulus Clouds • Cumulus clouds are puffy (like popcorn) • Often have noticeable vertical development • Cells can be rather isolated or they can be grouped together in clusters as shown • The base of a cumulus cloud can look like a stratus cloud if it is overhead. • Thick cumulus can make skies dark (filters out sun’s rays)

  11. Combining Shapes & Heights • Many different names of clouds combine: - a height (cirro-, alto-, nimbo) - a shape (cirrus, stratus, cumulus) • Let’s look at examples of these word combinations to describe different cloud types.

  12. Cirrocumulus • high cumulus clouds • Can see individual “puffy” features

  13. Cirrostratus • High-level stratus clouds • Not as thin as cirrus and less defined than cumulus

  14. Altocumulus • Mid level cumulus clouds

  15. Altostratus • Mid level stratus clouds

  16. Stratocumulus • Cross between stratus and cumulus

  17. Nimbostratus • Stratus clouds that are precipitating

  18. Cumulonimbus • Cumulus cloud with precipitation

  19. Orographic Clouds • Clouds can also be caused by mountains or hills • Result to air flowing up and over mountains which causes condensation to occur and clouds to form • Different types of clouds caused by orographic lift follow

  20. Cap Clouds • Air containing water vapor lifted until it is saturated, producing liquid water cloud droplets which can "cap" the summit. (cap cloud over Mt. Ranier)

  21. Lenticular Clouds • Lenticular means “like a lens” • Looks like flying saucers • Forms from air rising up a mountain

  22. Kelvin-Helmholtz Billows • Occurs in regions of strong density and velocity changes. (dynamics class)

  23. Contrails • Contrail is short for “condensation trails” • Formed from vapor contained in the exhaust of a jet engine when it condenses in cold air aloft

  24. A good web page to visit • A great website for clouds (where I got most of the lecture material) is: • http://vortex.plymouth.edu/cloud.html

  25. Announcements • Read Chapter 11 - How to Predict the Weather (pages 181 – 196) • Complete Homework 9 about cloud types • Only 4 more lectures!!! (So you can start getting ready to burn your books!) • If you have a question during the quiz or on the homework, you can ask me a question. I can’t help if you leave the answer blank.

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