Local Winds Inversions Cloud Vis Fog Flashcards
Katabatic winds
Usually during nighttime
Hill face cools and gravity helps pull cool air down hill
Anabatic winds
Generally after sunrise east facing slopes
Valley face heats and warm air blows up valley face
Opposing gravity so often less extreme than katabatic
Fohn wind
Moist air blows up hill and saturated dry air blows down hill warming at dalr resulting in warmer air on leeward side
Low pressure on leeward side sucks air downhill
Fohn wind conditions
Only occurs if enough moisture for salr to create temperature difference
Lee side
Gusty and turbulent
Reduced visibility due to dust and rock particles
Large scale interference
Mountain waves standing waves lee waves
Requirements:
Large mountain range
Wind at right angles to mountain range
Unstable lower atmosphere and stable upper atmosphere
Wind speed greater than or equal to 15 kts or more
Altocumulus lenticularis
Formed by wave
Appears stationary but constantly forming and dissipating
How to avoid mountain waves
Fly on windward coast
fly high
Use local knowledge
Rotor zones and streaming
Occur in lee of range
Essentially Eddie’s
Creates circular wind flow back towards mountains
Condensed air as it accelerates can form cloud
Clouds associated with mountain wave
Rotor cloud
Wave cloud
Cap cloud
Subsidence inversion
Occurs during anti cyclones (high pressure)
Upper level convergence low level divergence
Descending air is warming at a rate that makes it warmer than ascending air
Can create anti cyclonic gloom (clouds)
Radiation inversion
Air close to ground cools during night middle layer unaffected
Requires light wind and clear sky’s
Turbulence inversion
Top of friction layer
Induced by wind of at least 10kt
Air becomes turbulent and tumbling mixing cooling and warming eventually offsetting
Frontal inversion
Warm air forced over top of colder air
Inversion occurs at boundary between the two air masses
Five lifting mechanisms
Orographic lifting
Mechanical lifting
Thermal lifting (convection)
Slow widespread ascent
Frontal lifting
Cloud formation
Lifting air gets less pressure (cooling mechanism as less collisions because parcel expands)
Convective rising
ELR must exceed DALR
Always creates cu type cloud
Can be cb or tcu