1 / 25

ATOC 4720 class20

ATOC 4720 class20. Clouds and storms 1. Cloud morphology 2. Types of clouds 3. The air-mass thunderstorm. From class-19:. [1]. Thermoelectric effect in ice: T- degree C; V--mV. [2] Supercooled water in clouds. Class-19:. 3. Lightning and thunder.

duaa
Download Presentation

ATOC 4720 class20

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. ATOC 4720 class20 • Clouds and storms 1. Cloud morphology 2. Types of clouds 3. The air-mass thunderstorm

  2. From class-19: [1] Thermoelectric effect in ice: T- degree C; V--mV [2] Supercooled water in clouds

  3. Class-19: 3. Lightning and thunder Dielectric breakdown: V>3MV/m (dry) V>1MV/m Moist with 1mm in radius; Lightning: T--30,000K; Thunder: Shock waves;

  4. 1. Cloud morphology Clouds: Mechanisms of formation [1] Convective clouds: local ascent of warm, conditionally unstable air; 0.1-10km in diameters; Vertical velocity w: a few m/s; Liquid water or ice content:

  5. [2] Layer clouds: stratus Forced lifting of stable air: Examples: fog is forced lifted upwards; cold fronts lift warm air mass Hundres--thousands km; Lifting rates: a few cm/s; Water: a few tens Tens of hours

  6. stratus

  7. [3] Orographic clouds Forced lifting of air by hills or mountains Uplifting velocity depends on windspeed and direction, And mountain height. Can be a few m/s; Water: a few tens Can be transitory, or can stay for long if winds are Steady. Lee waves can also produce orographic clouds; http://www.faa.gov/and/AC0057/AC0057.HTM

  8. Orographic clouds

  9. [4] Advection fog: Cooling of air below its dew point due to warm air is Advected to a colder surface.

  10. Fog

  11. [5] Arctic sea-smoke (steam fog) Meeting of two parcels of air with different temperatures; both close to be saturated.

  12. Arctic sea-smoke

  13. [6] Funnel clouds Adiabatic expansion and cooling due to a rapid local Reduction in pressure. Tornadoes or water spouts.

  14. Funnel clouds

  15. Funnel clouds

  16. [7] Instabilities (Kelvin-Helmholtz instabilities) Strong wind-shear modify cloud shape;

  17. Billow clouds: K-H instability

  18. Types of clouds Many types: (International cloud Atlas) Cumulus: Stratus Cirrus Nimbus (combination) Cirrostratus

  19. Cumulus

  20. Cumulus tower

  21. Cumulonimbus

  22. Stratus

  23. Cirrus clouds

  24. Cirrostratus: halos

More Related