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