Atmospheric stability and cloud formation
This presentation is the property of its rightful owner.
Sponsored Links
1 / 21

Atmospheric Stability and Cloud Formation PowerPoint PPT Presentation


  • 121 Views
  • Uploaded on
  • Presentation posted in: General

Atmospheric Stability and Cloud Formation. RECAP. Mechanical equilibrium : stable, unstable, neutral. Adiabatic expansion/compression : no heat exchange. Adiabatic lapse rate Dry adiabatic lapse rate ~ 10 K/km Moist adiabatic lapse rate ~ 6 K/km Remember: Dry > Moist always

Download Presentation

Atmospheric Stability and Cloud Formation

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.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -

Presentation Transcript


Atmospheric stability and cloud formation

Atmospheric Stability and Cloud Formation


Recap

RECAP

  • Mechanical equilibrium: stable, unstable, neutral.

  • Adiabatic expansion/compression: no heat exchange.

  • Adiabatic lapse rate

    • Dry adiabatic lapse rate ~ 10 K/km

    • Moist adiabatic lapse rate ~ 6 K/km

    • Remember: Dry > Moist always

  • Environmental lapse rate.

  • Atmospheric stability:

    • Absolutely stable atmosphere

    • Absolutely unstable atmosphere

    • Neutrally stable atmosphere

    • Conditionally unstable atmosphere


Midchapter summary

Midchapter summary

  • The air temperature in a rising parcel of unsaturated air decreases at the dry adiabatic rate, while the air temperature in a rising parcel of saturated air decreases at the moist adiabatic rate.

  • The dry adiabatic rate and moist adiabatic rate of cooling are different due to the fact that latent heat is released in a rising parcel of saturated air.

  • In a stable atmosphere, a lifted parcel of air will be cooler (heavier) than the air surrounding it, and will tend to sink back to its original position.

  • In an unstable atmosphere, a lifted parcel of air will be warmer (lighter) than the air surrounding it, and will continue to rise upward, away from its original position.

  • The atmosphere becomes more stable (stabilizes) as the surface air cools and/or the air aloft warms.

  • The atmosphere becomes more unstable (destabilizes) as the surface air warms and/or the air aloft cools.

  • Layered clouds tend to form in a stable atmosphere, while cumuliform clouds form in an unstable atmosphere.


Stable atmosphere

Stable atmosphere


Unstable atmosphere

Unstable atmosphere


Sample test questions

Sample test questions

  • If the environmental lapse rate is 5 deg C per 1000 m and the temperature at the earth's surface is 25 deg C, then the air temperature at 2000 m above the ground is:

    • a.25 deg C

    • b.35 deg C

    • c.20 deg C

    • d.15 deg C

    • e.10 deg C


Sample test questions1

Sample test questions

  • Take the dry adiabatic lapse rate to be 10 deg C per 1000 m. A radiosonde has measured the temperature of the atmosphere to be 30 deg C on the ground and 15 deg C at an altitude of 1000 m. What can you say about the stability of the atmosphere?

    • The atmosphere is absolutely unstable

    • The atmosphere is conditionally unstable

    • The atmosphere is absolutely stable

    • The atmosphere is neutrally stable

    • This question cannot be answered without knowing the moist adiabatic lapse rate


How does the stability of the atmosphere change during the day

How does the Stability of the Atmosphere Change During the Day?

  • Daytime:

    • The sun heats the ground.

    • The boundary layer is heated from below.

    • The environmental lapse rate is steep.

    • The atmosphere can become unstable.

  • Morning and evening hours:

    • Radiation cooling results in temperature inversion.

    • The boundary layer is cooler than the air above.

    • The environmental lapse rate becomes less steep.

    • The atmosphere is stable.


Air stability

Air Stability

DAY

NIGHT

Adiabatic lapse rate

Environmental

lapse rate

Solar radiation

Altitude

IR cooling

20

30

The ground is warm

The ground is cool

Temperature [C]


Cloud formation

Cloud Formation


Convection and clouds

Convection and Clouds


Cumulus clouds

Cumulus Clouds


Atmospheric stability and cloud formation

Cumulus clouds


Formation of convective clouds

Formation of Convective Clouds

The surface air temperature is 35 C and the dew point is 25 C


Stability and cloud thickness

Stability and cloud thickness

  • A conditionally unstable atmosphere allows for saturated air to keep propagating upwards


Atmospheric stability and cloud formation

STABLE

UNSTABLE


Orographic uplift

Orographic uplift


Wave clouds

Wave clouds


Cap cloud

Cap cloud


Lenticular cloud

Lenticular cloud


Wave clouds1

Wave clouds


  • Login