Cloud Development & Classification


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Cloud Development & Classification

  1. 1. Atmospheric Basics Atmospheric Composition
  2. 2. Atmospheric Basics Atmospheric Composition Key Atmospheric Gases – The amount of water vapor in the atmosphere can be as much as four percent of the atmosphere or as little as almost zero. – Carbon dioxide, another variable gas, makes up under one percent of the atmosphere.
  3. 3. State of the Atmosphere Temperature Versus Heat  Temperature is a measurement of how rapidly or slowly molecules move.  Heat the transfer of thermal energy from one substance to another.  Heat is the transfer of energy that fuels atmospheric processes, while temperature is used to measure and interpret that energy.
  4. 4. State of the Atmosphere Temperature Versus Heat Measuring Temperature – Temperature can be measured in degrees Fahrenheit (°F), in degrees Celsius (°C), or in kelvins (K), the SI unit of temperature. – The Kelvin scale measures the number of kelvins above absolute zero, a point where molecular motion theoretically stops.
  5. 5. State of the Atmosphere Temperature Versus Heat Dew Point – The dew point is the temperature to which air must be cooled in order for it to be saturated to trigger condensation. a) Saturation is the point at which the air holds as much water vapor as it possibly can. b) Condensation cannot occur until air is saturated. – Condensation occurs when matter changes state from a gas to a liquid.
  6. 6. Cloud Formation
  7. 7. Moisture in the Atmosphere Cloud Formation  Buoyancy is the tendency for air to rise or sink as a result of differences in density.  There are 3 ways that clouds can form: 1) Clouds form when warm, moist air rises, expands, and cools in a convection current.  Condensation nuclei are small particles in the atmosphere around which cloud droplets can form.
  8. 8. Moisture in the Atmosphere Cloud Formation 2) Orographic lifting occurs when wind encounters a mountain and the air has no place to go but up.  The air expands and cools resulting in cloud formation.
  9. 9. Moisture in the Atmosphere Cloud Formation 3) Cloud formation occurs with the collision of air masses of different temperatures.  As warmer air collides with cooler air, the bulk of it will be forced to rise over the more-dense, cold air.  As the warm air cools, the water vapor in it condenses and forms a cloud.
  10. 10. Moisture in the Atmosphere Cloud Formation Stability – How rapidly any given mass of air cools determines its stability. – Stability is the ability of an air mass to resist rising. – The rate at which an air mass cools depends in part on the temperature of the surface beneath the air. – Air can become unstable if it is cooler than the surface beneath it. – If temperature conditions are right and the air mass rises rapidly, it can produce the type of clouds associated with thunderstorms.
  11. 11. Moisture in the Atmosphere Cloud Formation Latent Heat – As water vapor in the air condenses, heat is released. – The energy to change liquid water into a gaseous state is stored in the water vapor. – Latent heat is stored energy in water vapor that is not released to warm the atmosphere until condensation takes place. “Hidden – Heat” – The amount of water vapor present in the atmosphere is a significant source of energy because of the latent heat it contains.
  12. 12. Moisture in the Atmosphere Types of Clouds  The modern system groups clouds by the altitude at which they form and by their shape. – Low clouds typically form below 2000 m.
  13. 13. – Middle clouds form between 2000 m to 6000 m.
  14. 14. Altocumulus Lenticularis
  15. 15. – High clouds composed of ice crystals form above 6000 m.
  16. 16. The halo around the sun or moon is a layer of cirrus clouds made of ice crystals. These ice crystals act as tiny prisms, forming a white or sometimes colorful halo around the sun or moon. This cirro-stratus cloud often indicates an approaching warm front and an associated area of low pressure. Rain or snow will not always follow, but there is a higher probability of it after a halo is seen, and the brighter the circle, the greater the probability.
  17. 17. – Vertical development clouds spread throughout all altitudes at the same time.
  18. 18. Moisture in the Atmosphere Types of Clouds High clouds Wispy, feather-like, ice crystals. Puffy, cotton-like, Fair weather clouds Middle clouds Sheets, layers Low clouds Storm clouds
  19. 19. Types of Clouds Types of Clouds 3:17 minutes
  20. 20. Moisture in the Atmosphere Precipitation  Coalescence occurs when cloud droplets collide and join together to form a larger droplet.  When the droplet becomes too heavy to be held aloft, gravity takes over and it falls to Earth as precipitation.  Precipitation includes all forms of water, both liquid and solid, that fall from clouds including rain, snow, sleet, and hail.
  21. 21. Precipitation  When water vapor in the clouds becomes too heavy, it can fall as rain, sleet, snow, or hail.  Cloud droplets must first increase in size until gravity pulls them down.  If they pass through extremely cold layers of air, they can freeze and produce sleet  Snow is formed when water vapor changes directly into a solid.  Hail is formed when water droplets freeze in layers due to updrafts and downdrafts.
  22. 22. Moisture in the Atmosphere The Water Cycle  At any one time, only a small percentage of water is present in the atmosphere.  The water cycle is the constant movement of water between the atmosphere and Earth’s surface.
  23. 23. Water Cycle
  24. 24. 1. 2. 3. 4. 5. 6. Exit Ticket (Write Question Out Name the 5 atmospheric layers. Describe what the magnetosphere is. What are the 3 ways that energy in the atmosphere can be transferred on Earth? How are clouds classified? What are the prefixes to describe height: a) low b) middle c) high clouds? What are the prefixes to describe the shapes of clouds: a) wispy b) puffy c) layered d) storm