11-3 Moisture in the Atmosphere

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Title: 11.3 Clouds and Precipitation
Presentation transcript:

11-3 Moisture in the Atmosphere

Cloud formation Air generally contains the same amount of water vapor Warm air rising and cool air sinking Tendency to rise or sink is called what? Buoyancy Small particles in the atmosphere from which cloud droplets can formed are called what? Condensation Nuclei

Cloud formation Orographic lifting Cloud formation over a _______________ Air rises and cools

Cloud Stability Ability of an air mass to resist rising Unstable if air is cooler than surface beneath it Heat flows from the warmer surface to the cooler air Less dense air mass rises- if enough: produces thunderclouds

Latent Heat As water vapor condenses, ____________ is released The energy needed to change liquid to gas is stored and not released until condensation occurs Latent Heat Provides energy to a weather system increasing intensity

Cloud Formation Formed when rising air reaches LCL Water vapor condenses into droplets of liquid water or ice Takes place at different altitudes Fog: at earth’s surface

Chart Fill out the cloud type chart Height Shape Cirro: Cirrus: Alto: Cumulus: Strato: Stratus: Nimbus:

Cirrus: “hair” - whispy Alto: 2000m-6000m Cumulus: “pile”-puffy, lumpy Height Shape Cirro: 6000m+ Cirrus: “hair” - whispy Alto: 2000m-6000m Cumulus: “pile”-puffy, lumpy Strato: -2000m Stratus: “layer”- sheets Nimbus: “cloud”- low, grey

Clouds Low Clouds Water droplets If air stays cold, wind will spread it horizontally Stratocumulus Covers much of the sky at a given area

Clouds Middle Clouds Because of cooler temps, may be formed from liquid water or ice crystals Altocumulus, altostratus Mild precipitation

Clouds High Clouds Because of high altitude, clouds are from ice crystals Wispy and distinct appearance Varies in thickness

Clouds: Vertical Development If unstable, cumulus cloud will be warmer that air Will grow & rise while condensing water vapor warms air around it: Latent Heat May reach up to 18,000 meters Top forms ice crystals, wind spreads to an “Anvil” shape Thunderstorms

Precipitation When droplets collide, join together to form larger droplets Coalescence Gravity takes over and when heavy enough, droplet falls as precipitation Snow, rain, sleet, hail Water Cylce Precipitation  Runoff  Evaporation  Condensation