Wind Flashcards

1
Q

What measures surface wind

A

Anemometer

, 10m or 30ft agl

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2
Q

Gust

A

Sudden change in wind speed by 10kts in less than a min

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3
Q

Calm

A

1kt or less

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4
Q

Gale force

A

34-47kts

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5
Q

Storm force

A

48 - 63kts

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6
Q

Hurricane force

A

Greater than or equal to 64

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7
Q

Squall

A

Gust lasting more than 1 min

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8
Q

Lull

A

Sudden drop in wind speed

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9
Q

What happens to the surface wind in the northern hemisphere

A

Backed and slacks

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10
Q

Sea breeze wind speed

A

10 - 5kts

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11
Q

Anabatic

A

Winds going up the mountain, low pressure which is caused by convection, air comes in and goes up the mountain

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12
Q

Katabatic wind

A

Typical at night, surface cools, get denser, falls down the mountain

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13
Q

Geostrophic wind

A

The CF and PGF are equal and opposite and the wind gets deflected 90 degrees so wind travels parallel to the isobars

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14
Q

Ballots law

A

Back to the wind, low pressure will be on your left

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15
Q

Gradient wind

A

Wind coming out a high/low pressure

Coming out a high due to centrifugal for acting in the same direction, the the wind is faster

Wind around a low is slower due to the centrifugal force and the corolis acting the opposite direction

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16
Q

Deflection of the wind over the sea and % of the 3000ft wind

A

10 degrees, 70%

17
Q

Deflection of the wind over the land by day and % of the 3000ft wind

A

30 degrees, 50%

18
Q

Deflection of the wind over the land by night and % of the 3000ft wind

A

45 degrees, 25 %

19
Q

Diurnal variation

A

Durning the day, thermal activity on the surface causes fast high level air to get mixed with slow surface air to get a faster overall wind speed

Durning the night, less thermal air, no rising air, less mixing

20
Q

Sea breeze formation

A

Surface heating on the land causes a low pressure to form and thus causing a PGF, goes in opposite direction in the night

Wind gets deflected due to the CF

About 5 - 10kts, faster the speed, bigger the deflection

21
Q

Land breeze

A

Opposite to sea breeze

22
Q

Katabatic wind

A

Typical at night, surface cools, gets denser and falls down the mountain

23
Q

Example of the katabatic effect

A

The Bora, effects the adratic sea

24
Q

Example of valley winds

A

High pressure in the north Western Europe to low pressure in the south
PGF goes through the alps causing a Venturi
Strong relatively cold and dry wind

25
Q

Foehn wind

A

Stable, saturated air gets pushed up a mountain, cools, forms cap cloud, rains, dries, comes down the mountain as the DALR and is warmer

26
Q

Examples of foehn wind

A

Alps

Chinook in the rockies

27
Q

What happens in the med in winter

A

The low pressure over the med sea, drags the dry air from n Africa up

This mixes with the cold air from the European land mass and can cause intense storms

28
Q

Strong winds in the Southern Hemisphere

A

Roaring 40s
Furious 50s
Screaming 60s

29
Q

Doldrums

A

Calm surface conditions due to surface convergence at the ITCZ

30
Q

Harmattan

A

NE trade winds over w Africa

Dry sands can impact visibility

Strongest in jan due to the ITCZ moving downwards
Reduces viz up to 3000ft
Can extend to 10-15,000ft

31
Q

Pampero

A

S America

Cold polar air moves the flat land, increasing wind speed

Strongest winds occur early summer