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Cloud Types (Cirroform and cumuliform)
Cirriform - Thin wispy clouds of ice crystals. No sig weather comes from this type of cloud
Cumuliform - Puffy fair weather type clouds. Indicates unstable air and can develop into towering cumulus
Cloud Types (Nimbus clouds and lenticular)
Nimbus - Shallow and broad (nimbostratus) or tall/powerful (cumulionimbus)
Lenticular - Lens shape and indicates severe turb, common in mountainous areas
How does cloud formation occur?
Air is forced aloft and it cools to its saturation point. Water vapor condenses or sublimates creating clouds
What are some obstructions to visibility caused by clouds?
Rain
Sleet
Snow
Hail
Freezing Rain
Smoke
Caused by the suspension of combustible particles
Creates the illusion of being at greater distance than actual from runway resulting in lower approach
Haze
Caused by fine dry particles from fire
Creates the illusion of being at greater distance than actual from runway resulting in lower approach
Radiation fog
Forms over land on calm clear cool humid nights
Produced by condensation of water vapor due to condensation cooling. Dissipates in the morning quickly unless cloud layers form above
Advection fog
Forms when a low layer of warm moist air moves over a cooler surface
Most common under clouds skies along coastlines
Intensified by winds up to 15knots anything greater will dissipate it
Upslope fog
Moist stable air is forced up a slope
Similar to advection fog
Precipitation induced fog
Formed when warm rain/drizzle falls through a layer of cooler air near surface
Associated with warm fronts but can occur with slow moving cold/stationary
Ice fog
Formed in cold WX when temp is much below freezing
Caused by sublimation of water vapor directly into ice
Steam fog
Caused by cool air moving over warmer water
What is needed for the formation of a thunderstorm?
Unstable air
High moisture content of the air
Lifting action
Cumulus stage of TS
Lifting action indicating the vertical movement of air
Water vapor condenses as it rises releasing energy for further vertical growth
Mostly strong updrafts result no precip
Towering cumulus clouds form rapidly and reach mature stage in about 15minutes
Mature stage of TS
Starts when precip begins to fall at the surface
Precip becomes too heavy to support triggering downdrafts
Updrafts will still dominate in this stage
Lightning occurs here
Dissipating stage of TS
Downdrafts begin to disspiate the updrafts
Entire storm weakends
Storm is considered dead when rain is no longer produced
What are some of the hazards of TS?
Severe turb/wind shear - microbursts, downdrafts exceed 6000fpm
Icing - Severe or greater
Hail - occurs in mature dissipating stage
Low visibility - Caused by hail and precip
Formation of hail
Hail is formed by precipitation carried above and below the freezing layer by up and down drafts
Water than refreezes as the droplet is carried above the freezing level
Hail occurs in mature/disspiating stage
What are the types of icing
Clear
Mixed
Rime
Clear Ice
Formed by large water droplets that freeze slowly after striking the airframe forming a blanket
Accumulates quickly, adheres strong and difficult to remove
Avoid cumulus clouds, freezing rain, especially if below temp.
Rime Ice
Formed by small water droplets that freeze quickly to an aircraft
Rough, opaque cloudy appearance form on leading edge
Avoid stratiform clouds
Mixed Ice
Possess negative quality of rime and clear
What conditions are needed to cause icing
Contact surface temp below freezing
Moisture
Will snow cause icing?
Snow will not cause icing because its not liquid it has to be liquid and not already frozen
Icing reports
Trace - Only hazardous if experienced for over an hour
Light - Rate of accumulation may prevent a problem, use of de ice prevents it, doesn’t prevent a problem if de ice used
Moderate
Severe - Requires immediate altitude or route change
How should you fly in icing conditions differently
Turn around
Climb above/below clouds
Fly faster (5-10kts on appch)
Don’t change configuration