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Cumulus Clouds and Thunderstorms

Cumulus Clouds

  • puffy, “popcorn-like” clouds

  • cumulus humilis (humble):

    • fair weather

    • small

  • cumulus congestus (heap):

    • towering cumulus clouds

      • heating causes vertical updrafts

      • air parcels cool as they rise

      • excess water vapor condenses

      • latent heat released

      • causes more updrafts

Thunderstorms

  • cumulonimbus:

    • thunderstorm cloud

    • very large (tall), thick clouds

  • thunderstorm = cumulonimbus clouds with lightning and thunder (and commonly rain)

  • top of cloud is near top of troposphere

  • base of cloud is near the ground

  • strong updrafts and downdrafts (turbulent)

  • looks like a mushroom or an anvil (well-developed)

    • anvil can be 10s of mile in diameter

  • if very strong updrafts, then the dome of the cloud overshoots above the anvil

  • storm energy from temperature and humidity

Thunderstorm Occurrence

  • more commonly occur in:

    • tropical locations: abundant sunshine (heat) and moisture

    • late afternoons in the summer: most surface heating

  • also in regions with convergent winds and/or lifting

    • mountains

    • land/sea boundary

Thunderstorm Fuel

  • need constant inflow of warm, moist air or they die out

  • most thunderstorms use up fuel (warm, moist air) and choke on their exhaust (cool, dry air)

  • last only a half hour to an hour

AS

Cumulus Clouds and Thunderstorms

Cumulus Clouds

  • puffy, “popcorn-like” clouds

  • cumulus humilis (humble):

    • fair weather

    • small

  • cumulus congestus (heap):

    • towering cumulus clouds

      • heating causes vertical updrafts

      • air parcels cool as they rise

      • excess water vapor condenses

      • latent heat released

      • causes more updrafts

Thunderstorms

  • cumulonimbus:

    • thunderstorm cloud

    • very large (tall), thick clouds

  • thunderstorm = cumulonimbus clouds with lightning and thunder (and commonly rain)

  • top of cloud is near top of troposphere

  • base of cloud is near the ground

  • strong updrafts and downdrafts (turbulent)

  • looks like a mushroom or an anvil (well-developed)

    • anvil can be 10s of mile in diameter

  • if very strong updrafts, then the dome of the cloud overshoots above the anvil

  • storm energy from temperature and humidity

Thunderstorm Occurrence

  • more commonly occur in:

    • tropical locations: abundant sunshine (heat) and moisture

    • late afternoons in the summer: most surface heating

  • also in regions with convergent winds and/or lifting

    • mountains

    • land/sea boundary

Thunderstorm Fuel

  • need constant inflow of warm, moist air or they die out

  • most thunderstorms use up fuel (warm, moist air) and choke on their exhaust (cool, dry air)

  • last only a half hour to an hour