CLOUDS Flashcards
What gives us an indication that mountain wave in Mountain turbulence exist?
Lenticular clouds
Rotor clouds
Cap clouds
Banner, clouds
Lenticular clouds
Typically occur from 20,000 to 40,000 feet. Form in the crests of the waves, and can be very high and hundreds of miles long.
In PIREPS & METARS lenticular clouds will be reported as one of two types
ACSL
CCSL
Roll/rotor clouds
They will form downwind from each wave crest, and within the lower turbulent zone.
Possess the greatest amount of turbulence.
Can indicate presence of mountain waves
Cap cloud
These lie over the top of the mountain, and they will extend partially down the leeward slopes. This can indicate an extremely strong downdraft.
ACSL
Alto-cumulus, standing lenticular
CCSL
Cirro- cumulus standing lenticular
Winds around mountains
Anabatic winds
Katabatic winds
Glacier winds
Funnel winds
Anabatic winds
Formed as the sun word side of a mountain slope heats up, warm air rises.
Katabatic winds
A wind that flows down the slope of a mountain. It can happen in shaded or snow-covered areas.
Glacier winds
Extreme katabatic winds. They are caused by glaciers which can produce areas of extreme cooling.
Funnelling winds
Winds, which are deflected around large single mountain peaks, or through the valleys of mountain ranges.
When should a light aircraft stay out of the mountains?
When the wind speed at the level of the mountain peak is 20 KT or greater
CB
Low cloud
Cumulonimbus
Thunder and lightning associated. Fueled by vigorous convective updrafts. Tops of these clouds can reach 60,000ft.
TCU
Low cloud
Towering cumulonimbus
Growing cumulus clouds. On the way to becoming a cumulonimbus
CU
Low cloud
Cumulus
Appearance of floating cotton or popcorn popping. Lifetime 5-40mins. Indicates the pressure of significant vertical currents at low levels without precip. With proper conditions they can develop into TCU, And than CB a powerful thunderstorm.