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)
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
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)
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.
Cirrus Photo
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
Stratus Photo
Fog (Stratus on Ground) Photo
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)
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.
Cirrocumulus
• high cumulus clouds
• Can see individual “puffy” features
Cirrostratus
• High-level stratus clouds
• Not as thin as cirrus and less defined than
cumulus
Altocumulus
• Mid level cumulus clouds
Altostratus
• Mid level stratus clouds
Stratocumulus
• Cross between stratus and cumulus
Nimbostratus
• Stratus clouds that are precipitating
Cumulonimbus
• Cumulus cloud with precipitation
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
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)
Lenticular Clouds
• Lenticular means “like a lens”
• Looks like flying saucers
• Forms from air rising up a mountain
Kelvin-Helmholtz Billows
• Occurs in regions of strong density and
velocity changes. (dynamics class)
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
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
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.

Cloud Types (materi atmosfer Olimpiade kebumian)

  • 1.
    Lecture 9 (11/04) METR1111 Cloud Types
  • 2.
    Cloud Classification • In1803, 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 cloudstell 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.
  • 7.
    Stratus Clouds • Stratusclouds 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.
  • 9.
    Fog (Stratus onGround) Photo
  • 10.
    Cumulus Clouds • Cumulusclouds 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 cumulusclouds • Can see individual “puffy” features
  • 13.
    Cirrostratus • High-level stratusclouds • Not as thin as cirrus and less defined than cumulus
  • 14.
  • 15.
  • 16.
  • 17.
    Nimbostratus • Stratus cloudsthat are precipitating
  • 18.
  • 19.
    Orographic Clouds • Cloudscan 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 • Aircontaining 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 • Lenticularmeans “like a lens” • Looks like flying saucers • Forms from air rising up a mountain
  • 22.
    Kelvin-Helmholtz Billows • Occursin regions of strong density and velocity changes. (dynamics class)
  • 23.
    Contrails • Contrail isshort for “condensation trails” • Formed from vapor contained in the exhaust of a jet engine when it condenses in cold air aloft
  • 24.
    A good webpage 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 Chapter11 - 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.