Chapter 5: Clouds
Fog: A cloud in contact with the ground
Fog forms when condensation begins to dorm on less active nuclei
Usually when the RH is closer to 100%
Fog droplets grow in size and eventually fall to the ground
Fog is formed in two ways:
Cooling the air to it’s saturation point (dew point)
Melting and evaporation (adding more vapor content to the atmosphere)
Fog is maintained by:
Forming new “fog droplets”
Adding moisture to the atmosphere
puddles, lakes, recent rains/snow melt, etc.
Clouds
Stratus - “Layers”
Cumulus - “Heap”
Cirrus - “Curl of hair”
Nimbus - “Violent Rain”
Nimbostratus - rain clouds that are layered
Cumulonimbus - rain clouds that show significant vertical growth
4 Primary groups (height levels)
High-level Clouds
Form above 20,000 feet
Almost exclusively “ice crystal” clouds
Little moisture available - thin clouds
Cirrus Clouds
Most common high cloud
Thin and wispy clouds
Move from west to east
Indicate the wind direction at elevation
Generally fair & pleasant weather
Cirrocumulus Clouds
Small, rounded, white puffs
Isolated, or in rows:
Isolated - little piles of sand
Rows - rippling appearance; scales of fish
Seldom cover a small portion of a sky
Cirrostratus Clouds
Thin, sheet-like high clouds
So thin, sun & moon can shine through
Usually produce a “halo”
Form ahead of approaching storms:
Good predictor of rain or snow withing 12-24 hours
Middle-level Clouds
Cloud Bases: 6,500 - 23,000 feet
Water droplets and ice crystals
Thicker clouds that sometime dim the sun
Altocumulus Clouds
Gray, puffy masses - waves or bands
Can be an “overcast cloud”
Sometimes look like little “castles”
castellanus
Precursor of summer afternoon thunderstorms
Altostratus Clouds
Gray, bluish color - covers the sky
A “milky” look
sun is dimly visible
One big (thin) blanket
Won’t see any shadows
Forms ahead of storms producing widespread rain
As the clouds start to lower, the percentage of precipitation increases
Low-level Clouds
Cloud Bases: Below 6,500 feet
Comprised of water droplets (mostly)
Gloomy looking sky - often in winter
Stratocumulus Clouds
Low and lumpy clouds
Appear in rows or patches
Blue sky is sometimes visible
“Precip-Free” type of cloud - usually
Easily confused with altocumulus
Nimbostratus Clouds
Dark gray, “wet-looking” cloud
Associated with continuous precipitation
(drizzle, rain and snow)
Intensity of precipitation is always light
Very low-lying clouds
although their tops can exceed 10,000 feet
Visibility is quite poor with nimbostratus'
due to rain and fog
Scud Clouds
Can sometimes break apart in the wind
Stratus Cloud
Uniform, grayish cloud
Covers the entire sky
Resembles fog
although doesn’t touch the ground
Light precipitation can fall from stratus
usually just drizzle or flurries
Vertically Developed Clouds
Cloud bases: 1,000 - 5,000 feet
Cloud tops: 5,000 - 80,000 feet
Comprised of water and ice
Cumulus Clouds
Variety of shapes - cotton ball
Sharp outlines and puffy
Base is light and gray
“Detached Clouds” and have dome-like tops
Show slight vertical growth
Cumulus Humilis
Fair weather clouds
Cumulonimbus Clouds
Continuously growing cumulus cloud
This is a thunderstorm
Base may start at 2,000 feet
Tops may grow to 40,000 feet and higher
Vertical growth depends to updrafts and downdrafts inside the thunderstorm
The taller a cloud grows, the more problems the cloud will have (severe weather
Cool the air, condense the air, becomes a cloud
Anvil Clouds
Flat anvil top of a tall cumulonimbus cloud
Castellanus Cloud
Tower-like vertical extension
Lenticular - shaped like a dome that hovers over a mountain