Wind Shear
can be found on all sides of a thunderstorm cell and in the downdraft directly under the cell
4135
constant tailwind shears to a calm wind
- airspeed and pitch increase
- a tendency to go above the glide slope
note: same effect when a tailwind shears to a headwind
4727
headwind shears to a constant tailwind
- airspeed decreases
- the nose pitches down
- aircraft will begin to drop below the glide slope
- thrust must be increased initially to resume normal approach speed
- thrust is reduced as the airspeed stabilizes, vertical speed increases
- indicated airspeed decreases and then increases to approach speed.
4739 4755
LLWS
Low-level wind shear may result from a frontal passage, thunderstorm activity, or low-level temperature inversion
4150