High Pressure
Wind direction
Anticlockwise
Low Pressure
Wind direction
Clockwise
Coriolis Effect
+ Winds from equator move East in front of spin direction
+ Winds from poles move West (not spinning as fast)
Pressure Gradient
The rate at which pressure changes over a given horizontal distance determines the Pressure Gradient
Greater pressure gradient
= faster moving air
= high winds
What happens when a High Pressure is really close to a Low Pressure ?
A High wants to be a Low
Greater pressure gradient
= faster moving air
= high winds
high pressure air quickly moves to low pressure area
High pressure & low pressure
In North
&
South Hemisphere
North
- Low Pressure = Anti-Clockwise
- Hight Pressure = Clockwise
South
- Low Pressure = Clockwise
- Hight Pressure = Anti-Clockwise
Gradient Flow
Gradient flow = wind following Isobars around pressure system (clockwise or anti-clockwise
Wind behaviour = Coriolis effect & pressure gradient force
Wind speed low = Stronger Pressure gradient force (goes out of high into a low)
Winds increase = Follows isobars more
Geostrophic Flow
Buy Ballot’s Law
If you stand with your back to the wind in the southern hemisphere, the low pressure will always be on the right
If QNH at destination aerodrome is less than departure point where is wind coming from ?
Wind coming from RIGHT
If QNH at destination aerodrome is same than departure point where is wind coming from ?
Flying along isobar
Wind either TAIL or HEAD wind
What hight does Surface friction effect wind
below 3000 ft
Direction of Surface Winds in southern hemisphere
Always to the right
wind in L pressure turns Right into Low
wind in H pressure turns Right into Low
Both deflected across Isobars into L Pressure system
Near the surface what force on wind is stronger
Near surface = more friction = lower wind speed
Pressure Gradient stronger
Pulls winds across isobars
Veers RIGHT
Backing wind =
BACKING to the LEFT
Veering wind =
VEERING to the RIGHT
how much does wind speed drop & direction Veer
Over Land =
Over Sea =
Over Land = 2/3 -> Veers 30’
Over Sea = 1/3 -> Veers 10’
What is a Squall
What is a Gust
Sudden change of smaller magnitude & duration
Rapid increase in wind strength followed by a lull back to average speed
What is Wind Shear
Could be different
+ Speeds
+ Directions
+ Temperatures
Types of Wind Shear
&
When they occur
Horizontal -> up / down drafts in mature TS
Vertical -> surface inversions - cold surface air - hot air above
Sea Breeze
1 ) Land heats during day (vs slow warming water)
2 ) Warm land air rises (creates L pressure)
3 ) Cool sea air comes onto land
Land Breeze
1 ) Land cools at night
2 ) Warm air over ocean rises (water slow to cool)
3 ) Air blows out to sea
Katabatibc winds
Conditions =
= Night
= Steep land descent
= Clear skies (allowing max land heat loss)
= Cool surface air & Warm surrounding air