Winds Flashcards
What measures wind?
Anemometer
33ft (10m) AGL
Wind Vane
Wind Strengths
Calm = 1kt or less
Gale Force Winds = 34kt to 47kt
Storm force winds = 48kt to 63kt
Hurricane force winds = 64kt
Definition of a gust
A variation of 10kt or more above average wind speed lasting a minute
Definition of gustiness
Difference between min/max gust speeds
Definition of a lull
Sudden drop in wind speed
What is a variable wind
A variation of 60 degree or more in wind direction
Wind Reporting
METARS/TAFS = Degrees true (reported avg 10 mins)
ATC = Degrees Magnetic (report average 2mins)
PGF
Pressure Gradient Force - High to low
Coriolis (Geostrophic Force)
Rotation of earth deflects the winds to the right in NH
Rotation of earth deflects the winds to the left in SH
Coriolis is influenced by
Latitude - Higher latitudes more deflection in wind
Density - greater density more deflection
Wind speed - higher wind speed more deflection
Geostrophic Winds
PGF + CORIOLIS
Balance in speed/direction
Parallel to straight isobars
Gradient Wind
PGF + Coriolis + Centrifugal forces
Blows along curved isobars
Gradient Wind around low pressure
Centrifugal force opposed the PGF therefore reducing wind speed.
Reduces Coriolis force and then leading to flowing parallel to isobars
Gradient in a depression is lower than the Geostrophic winds (overread)
Gradient Wind around high pressure
Centrifugal force acts in same direction as PGF force wind speeds increase.
Gradient wind is greater than the Geostrophic winds (underread)
Friction Layer
SFC to 2000/3000ft
Affected by terrain/wind speed/stability
Night time layer reduces from around 1500ft
Surface Wind Model
Winds back in NH due to reduced Coriolis
Winds Veer in SH due to decreased Coriolis effect
NH back and slack meaning
Heading reduces/speed reduces as you descend into surface friction layer
Heading veers and increases as you flight out of surface friction layer
Surface Friction comparison between sea and land
Over land 50% decrease in wind speed in surface layer
Over sea 30% decrease in wind speed in surface layer
Over land direction changes by 30 degrees
Over sea direction changes by 10/15 degrees
Diurnal Variation on surface winds
In afternoon strongest winds therefore more Coriolis force less deviation from Coriolis as surface winds stronger
At dawn winds are the weakest and therefore surface winds will deviate more in the surface friction layer more
Wind Shear is measured in
Horizontal wind shear - knots per 1000ft
Vertical wind shear - knots per 100ft
Low around a low and high around a high meaning
Gradient wind is less than the Geostrophic wind in a low pressure system
Gradient wind is higher than the Geostrophic wind in a high pressure system
Gradient winds flows around
Curved Isobars
Geostrophic winds flow parallel to
Straight isobars
“NH back and slack” meaning
In the northern hemisphere descending down into friction layer the wind direction will back and speeds will reduce
Dangers of flying close to the ITCZ
Showers
Strong winds
Thunderstorms at noon