Winds Flashcards

(26 cards)

1
Q

High Pressure
Wind direction

A

Anticlockwise

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2
Q

Low Pressure
Wind direction

A

Clockwise

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3
Q

Coriolis Effect

A
  • the faster moving object will push object (wind) out in front of where its going
  • Equator is moving faster then poles

+ Winds from equator move East in front of spin direction
+ Winds from poles move West (not spinning as fast)

  • Particles moving across a rotating surface - path it traces is deflected
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4
Q

Pressure Gradient

A

The rate at which pressure changes over a given horizontal distance determines the Pressure Gradient

Greater pressure gradient
= faster moving air
= high winds

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5
Q

What happens when a High Pressure is really close to a Low Pressure ?

A

A High wants to be a Low

Greater pressure gradient
= faster moving air
= high winds

high pressure air quickly moves to low pressure area

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6
Q

High pressure & low pressure

In North
&
South Hemisphere

A

North
- Low Pressure = Anti-Clockwise
- Hight Pressure = Clockwise

South
- Low Pressure = Clockwise
- Hight Pressure = Anti-Clockwise

  • A low is always in the direction of earths rotation
    + looking upwards on south pole - its rotation is clockwise
    + looking downwards on north pole - its rotation is anti-clockwise
  • both cyclonic rotation
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7
Q

Gradient Flow

A

Gradient flow = wind following Isobars around pressure system (clockwise or anti-clockwise

Wind behaviour = Coriolis effect & pressure gradient force

  • If pressure gradient stronger = curves right in a low P system
    If Coriolis Effect stronger = flow curves left in High P system

Wind speed low = Stronger Pressure gradient force (goes out of high into a low)

Winds increase = Follows isobars more

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8
Q

Geostrophic Flow

A
  • Isobars are straight
  • Exact balance between gradient flow & Coriolis flow
  • Wind swings neither left or right
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9
Q

Buy Ballot’s Law

A

If you stand with your back to the wind in the southern hemisphere, the low pressure will always be on the right

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10
Q

If QNH at destination aerodrome is less than departure point where is wind coming from ?

A

Wind coming from RIGHT

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11
Q

If QNH at destination aerodrome is same than departure point where is wind coming from ?

A

Flying along isobar
Wind either TAIL or HEAD wind

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12
Q

What hight does Surface friction effect wind

A

below 3000 ft

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12
Q

Direction of Surface Winds in southern hemisphere

A

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

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13
Q

Near the surface what force on wind is stronger

A

Near surface = more friction = lower wind speed

Pressure Gradient stronger

Pulls winds across isobars
Veers RIGHT

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14
Q

Backing wind =

A

BACKING to the LEFT

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15
Q

Veering wind =

A

VEERING to the RIGHT

16
Q

how much does wind speed drop & direction Veer
Over Land =
Over Sea =

A

Over Land = 2/3 -> Veers 30’
Over Sea = 1/3 -> Veers 10’

17
Q

What is a Squall

A
  • Wind Change by at least 16 kt
  • Reach 22 kt or more
  • Sustained for more then 1 min
18
Q

What is a Gust

A

Sudden change of smaller magnitude & duration
Rapid increase in wind strength followed by a lull back to average speed

19
Q

What is Wind Shear

A
  • 2 adjacent airstreams - that don’t mix
  • boundary of airstreams becomes turbulent

Could be different
+ Speeds
+ Directions
+ Temperatures

20
Q

Types of Wind Shear
&
When they occur

A

Horizontal -> up / down drafts in mature TS

Vertical -> surface inversions - cold surface air - hot air above

21
Q

Sea Breeze

A

1 ) Land heats during day (vs slow warming water)
2 ) Warm land air rises (creates L pressure)
3 ) Cool sea air comes onto land

  • Strongest Mid afternoon
22
Q

Land Breeze

A

1 ) Land cools at night
2 ) Warm air over ocean rises (water slow to cool)
3 ) Air blows out to sea

  • More gentle sea breeze
    (temp diff isn’t as great)
23
Q

Katabatibc winds

A

Conditions =
= Night
= Steep land descent
= Clear skies (allowing max land heat loss)
= Cool surface air & Warm surrounding air

  • Air is denser & heavier then surrounding air
  • Gravity down land = Strong winds
  • Strongest at dawn
24
Anabatic Winds
- During the day - Wind blows up sloping terrain - Weak winds (have to go up hill) - During Afternoons 1 ) Land heats 2 ) Warm air rises 3 ) Cool air bows up terrain to replace hot air
25
Low Level Jet Streams
- Form in tropical inland areas E.g. - High Pressure system moves east across Aust - Lower level air is trapped between centre of H pressure & mountain ranges - Makes Isobars crowd together - Increases surface pressure gradient -> wind speed increases