Winds Flashcards

1
Q

What measures wind?

A

Anemometer
33ft (10m) AGL

Wind Vane

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2
Q

Wind Strengths

A

Calm = 1kt or less
Gale Force Winds = 34kt to 47kt
Storm force winds = 48kt to 63kt
Hurricane force winds = 64kt

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3
Q

Definition of a gust

A

A variation of 10kt or more above average wind speed lasting a minute

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4
Q

Definition of gustiness

A

Difference between min/max gust speeds

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5
Q

Definition of a lull

A

Sudden drop in wind speed

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6
Q

What is a variable wind

A

A variation of 60 degree or more in wind direction

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7
Q

Wind Reporting

A

METARS/TAFS = Degrees true (reported avg 10 mins)

ATC = Degrees Magnetic (report average 2mins)

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8
Q

PGF

A

Pressure Gradient Force - High to low

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9
Q

Coriolis (Geostrophic Force)

A

Rotation of earth deflects the winds to the right in NH
Rotation of earth deflects the winds to the left in SH

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10
Q

Coriolis is influenced by

A

Latitude - Higher latitudes more deflection in wind
Density - greater density more deflection
Wind speed - higher wind speed more deflection

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11
Q

Geostrophic Winds

A

PGF + CORIOLIS

Balance in speed/direction
Parallel to straight isobars

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12
Q

Gradient Wind

A

PGF + Coriolis + Centrifugal forces
Blows along curved isobars

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13
Q

Gradient Wind around low pressure

A

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)

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14
Q

Gradient Wind around high pressure

A

Centrifugal force acts in same direction as PGF force wind speeds increase.

Gradient wind is greater than the Geostrophic winds (underread)

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15
Q

Friction Layer

A

SFC to 2000/3000ft
Affected by terrain/wind speed/stability
Night time layer reduces from around 1500ft

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16
Q

Surface Wind Model

A

Winds back in NH due to reduced Coriolis

Winds Veer in SH due to decreased Coriolis effect

17
Q

NH back and slack meaning

A

Heading reduces/speed reduces as you descend into surface friction layer

Heading veers and increases as you flight out of surface friction layer

18
Q

Surface Friction comparison between sea and land

A

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

19
Q

Diurnal Variation on surface winds

A

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

20
Q

Wind Shear is measured in

A

Horizontal wind shear - knots per 1000ft
Vertical wind shear - knots per 100ft

21
Q

Low around a low and high around a high meaning

A

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

22
Q

Gradient winds flows around

A

Curved Isobars

23
Q

Geostrophic winds flow parallel to

A

Straight isobars

24
Q

“NH back and slack” meaning

A

In the northern hemisphere descending down into friction layer the wind direction will back and speeds will reduce

25
Q

Dangers of flying close to the ITCZ

A

Showers
Strong winds
Thunderstorms at noon