lecture recording on 27 February 2025 at 15.13.13 PM
Overview of Weather Concepts
The upcoming exam will cover chapters on cloud types and precipitation processes, but thunderstorms may not be included.
It’s suggested to study previous notes and feel free to ask questions during the next class.
Cloud Types
General Classification
Cloud names are based on altitude, vertical motion, and appearance.
Three layers of clouds: high, middle, and low clouds.
High Clouds (Cirrus)
Cirrus Clouds
Wispy appearance, resembling a horse's tail.
Composed of ice crystals; conditions lead to streaks forming due to wind currents.
Low Clouds (Stratus, Nimbostratus, Cumulus)
Stratus Clouds
Layered, uniform gray clouds that can bring rain (nimbostratus).
Form from slow lift over large areas, common with cold fronts.
Cumulus Clouds (Fair Weather Clouds)
Tall and puffy, associated with buoyant air parcels.
Growth occurs when latent heat is released once condensation level is reached.
Can become Cumulonimbus Clouds, which are associated with thunderstorms and precipitation.
Middle Clouds (Altostratus, Altocumulus)
Altostratus Clouds
Found halfway through the troposphere and often have a layered appearance.
Altocumulus Clouds
Puffy but larger than typical cumulus; can be mistaken for high or low clouds.
Other Cloud Types
Cirrostratus
Thin, covering a large area, often causing glare through sunlight.
Cirrocumulus
High, small, and puffy clouds indicative of instability.
Stratocumulus
Low, broken layer of clouds that can appear puffy.
Cloud Coverage Conditions
Coverage Classification
Clear: 0-5% coverage, no clouds.
Few Clouds: 5-25% visibility of clouds.
Scattered Clouds: 25-50% coverage, often termed partly cloudy.
Mostly Cloudy (Broken): 50-87% coverage.
Overcast: 87-100% coverage, completely clouded sky.
Obscured: Visibility is limited due to conditions like fog or dust storms.
Weather Reporting Codes (METAR)
Sky conditions are reported in a coded format (METAR) which gives pilots and meteorologists a concise weather report.
Example: Lubbock METAR describes cloud coverage and other weather conditions in a standardized three-letter code system.
Precipitation Processes
Hydrometeors
Definition: Any water particle (liquid or ice) that has condensed from vapor in the atmosphere, including clouds and rain.
Growth Stages
Cloud condensation nuclei (CCN) grows into droplet sizes ranging from 10-50 micrometers before turning into raindrops (>100 micrometers).
Larger droplets eventually develop into precipitation.
Collision-Coalescence Process
Grow larger droplets by colliding with and coalescing smaller droplets in clouds.
The rate of coalescence is directly influenced by the size; larger drops fall faster and 'collect' smaller droplets.
This mechanism occurs in clouds with significant depth such as cumulonimbus clouds, which are capable of producing rainfall.
Raindrop Characteristics
As raindrops fall, they undergo deformation due to air drag; smaller droplets remain round while larger ones can become hamburger-shaped before breaking apart.
Summary and Next Steps
Focus on distinguishing types of clouds, understanding conditions for precipitation, and recognizing cloud coverage conditions.
Utilize visual resources to analyze cloud types in real scenarios.