1 / 34

Atmospheric Moisture

Atmospheric Moisture. Moisture, Clouds, and Precipitation. Humidity Global Precipitation Lifting Mechanisms Precipitation Processes Big Question: What Causes Air to Precipitate?. Global Precipitation. After Saturation Occurs the Air Must Release Extra Water as Fluid.

lynde
Télécharger la présentation

Atmospheric Moisture

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Atmospheric Moisture

  2. Moisture, Clouds, and Precipitation • Humidity • Global Precipitation • Lifting Mechanisms • Precipitation Processes Big Question: What Causes Air to Precipitate?

  3. Global Precipitation

  4. After Saturation Occurs the AirMust Release Extra Water as Fluid Water forms on the outside of a cold glass as the cold Air surrounding the glass chills the air to the Dew Point Temperature The resulting water is not from the glass, the water is from condensation of moisture in the air around the glass

  5. Forms of Precipitation • Precipitation (pre-sip-uh-tay-shun) is any form of water that falls to the Earth's surface.

  6. Types of Precipitation • The type of precipitation that falls to the ground depends upon the formation process and the temperatures of the environment between the cloud and the surface

  7. Can you name the different types of precipitation? • Rain • Snow • Hail • Sleet • Freezing Rain

  8. Precipitation Types / Properties

  9. Rain • Rain develops when growing cloud droplets become too heavy to remain in the cloud and as a result, fall toward the surface as rain

  10. Rain can also begin as ice crystals that collect each other to form large snowflakes As the falling snow passes through the freezing level into warmer air, the flakes melt

  11. Rain from snow!

  12. Snow • Snow is formed when ice crystals form from water vapor that is in the clouds directly above your heads! • This process is called sublimation

  13. Snowflakes and Temperature Snow crystal images from an electron microscope

  14. Hail • Hail is formed when updrafts carry raindrops upwards into extremely cold areas of the atmosphere

  15. Hail • There the raindrops merge and freeze. When the frozen clumps get to heavy they fall to earth

  16. Sleet • Sleet is frozen raindrops. Sleet begins as rain or snow and falls through a deep layer of cold air that contains temperatures below freezing that exist near the surface.

  17. Sleet • Rain that falls through this extremely cold layer has time to freeze into small pieces of ice

  18. Freezing Rain • Freezing rain is falling rain that cools below 0°C, but does not turn to ice in the air • The water is “supercooled”

  19. When the drops hit anything they instantly turn to ice!

  20. Measuring Precipitation

  21. Measuring Rain w/ Standard Gauge Standard rain gauge uses a funnel to collect rain and then stores it in a narrower tube, so that the gauge detection is amplified 10-fold. The 50 cm long tube, when filled, represents only 5 cm of total rainfall. Figure 8.27

  22. Measuring Rain w/ Recording Gauge Figure 8.28 Tipping bucket and weighing rain gauges record precipitation rate at shorter time intervals, providing rain intensity data. Snow intensity can be measured with depth recorders, or accumulated totals with measuring sticks.

  23. Snow depth • Snow can be measured as an actual depth by sticking a measuring stick into it • This is not reliable as the depth will change the next place you measure • Depth will depend on the type of snowflakes that fall (how fluffy they are)

  24. Equivalent rain water depth • Usual conversion is 10 to 1 • 10cm of snow = 1cm of rain • (or 10” snow = 1” rain) • But very variable and depends on type of snow and how long it’s been settling

  25. Annual Precip

  26. Annual snowfall

  27. Quiz Time

  28. Ready? • Nuclei for the formation of rain drops can be small particles of: A) salt, B) smoke, C) dust, D) all the above • Which of these cloud types is not based on the clouds shape: A) stratus, B) nimbus, C) cumulus, D) cirrus

  29. 3. Mid elevation clouds between 2000 and 6000m: A) nimbus, B) alto, C) cirro, D) strato 4. This form of precipitation is supercooled: A) rain, B) snow, C) sleet, D) freezing rain

  30. 5.This form of precipitation stays frozen all the way to the ground: A) rain, B) snow, C) sleet, D) freezing rain Let’s see how you did!

  31. The Answers! 1. D 2. B 3. B 4. D 5. B

  32. Summary • Precipitation (Rain, Snow, Sleet) • When air is substantially cooled below the dew point, large droplets or ice crystals form and may fall if large enough.

More Related