050.02 Wind Flashcards

1
Q

The pressure gradient force acts (parallel/perpendicular) to the isobars towards the (lower/higher)​ pressure.

A

The pressure gradient force acts (perpendicular) to the isobars towards the (lower) pressure.

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2
Q

Surface wind is measured (2 / 8-10)​ m above the ground on a mast with an anemometer.

A

Surface wind is measured (8-10) m above the ground on a mast with an anemometer.

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3
Q

Cold depressions become (stronger/weaker)​ with height.

A

Cold depressions become (stronger) with height.

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4
Q

The average height of the jet core within a sub-tropical jet stream is (…)​ ft.

A

The average height of the jet core within a sub-tropica jet stream is (40 000) ft.

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5
Q

Conditions most favourable to the formation of mountain waves are (stable/unstable) air, wind speed (below/above) 20 kts blowing (across/parallel) the ridge.

A

Conditions most favourable to the formation of mountain waves are (stable) air, wind speed (above) 20 kts blowing (across) the ridge.

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6
Q

Minimum speed for a wind to be classified as a jet stream is (…) ​kts.

A

Minimum speed for a wind to be classified as a jet stream is (60) kts.

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7
Q

In the Northern Hemisphere, the Coriolis force deflects the wind to the (left/right)​. Coriolis force is (zero/maximum)​ at the equator.

A

In the Northern Hemisphere, the Coriolis force deflects the wind to the (right). Coriolis force is (zero) at the equator.

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8
Q

The two jetstreams that exists all year around are the (…) jet and the (…) jet.

A

The two jetstreams that exists all year around are the (polar front) jet and the (sub-tropical) ​jet.

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9
Q

Divergence in the upper air that is greater than the convergence in the friction layer results, near the surface, in (rising/falling) pressure and likely (formation/dissipation) ​of cloud.

A

Divergence in the upper air that is greater than the convergence in the friction layer results, near the surface, in (falling) pressure and likely (formation) of cloud.

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10
Q

State the two seasonal jetstreams, their direction, the season they occur and their approximate latitude.

A

State the two seasonal jetstreams, their direction, the season they occur and their approximate latitude:

  • Arctic jet; westerly; occurs in winter months; around 60°N
  • Equatorial jet; easterly; occurs during summer months; around 15°N
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11
Q

The average height of the jet core within a polar front jet stream is (…)​ ft.

A

The average height of the jet core within a polar front jet stream is (30 000) ft.

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12
Q

Geostrophic force is strongest close to the (equator/poles)​.

A

Geostrophic force is strongest close to the (poles).

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13
Q

The wind, which blows when pressure gradient and coriolis forces are in balance is the (…)​ wind.

A

The wind, which blows when pressure gradient and coriolis forces are in balance is the (Geostrophic) wind.

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14
Q

The worst area for CAT in the vicinity of the polar jet stream is normally located (in/above/below) the core on the (tropical/depression)​ side.

A

The worst area for CAT in the vicinity of the polar jet stream is normally located (below) the core on the (depression) side.

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15
Q

The average height of the jet core within an arctic jet stream is (…)​ ft.

A

The average height of the jet core within an arctic front jet stream is (20 000) ft.

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16
Q

Wind that has changed anti-clockwise in direction can be said to have (backed/veered)​.

A

Wind that has changed anti-clockwise in direction can be said to have (backed).

17
Q

Using a cup anemometer, (…) ​can be measured.

A

Using a cup anemometer, (wind speed) can be measured.

18
Q

Warm depressions become (stronger/weaker)​ with height.

A

Warm depressions become (weaker) with height.

19
Q

Warm anti-cyclones become (stronger/weaker)​ with height.

A

Warm anti-cyclones become (stronger) with height.

20
Q

On the Northern hemisphere over sea, surface winds are (backing/veering) by about (…)° and speed slows down to about (…)​% of the 2000 ft geostrophic winds.

A

On the Northern hemisphere over sea, surface winds are (backing) by about (10)° and speed slows down to about (70)% of the 2000 ft geostrophic winds.

21
Q

The approximate ratio between the height and widt for a jetstream cross section is in the range of 1:(1/10/100/1000)​.

A

The approximate ratio between the height and widt for a jetstream cross section is in the range of 1:(100).

22
Q

Turbulence caused by the friction of air flowing over the earth’s surface is (…) ​turbulence.

A

Turbulence caused by the friction of air flowing over the earth’s surface is (mechanical) turbulence.

23
Q

In the Northern hemisphere, the winds flow clockwise around a (LOW/HIGH) pressure area, (cyclonic/anti-cyclonic) flow.

A

In the Northern hemisphere, the winds flow clockwise around a (HIGH) pressure area, (anti-cyclonic) flow.

24
Q

A cloud type frequently associated with jet streams is a (…) cloud band on the (equatorial/polar)​ side of the jet stream.

A

A cloud type frequently associated with jet streams is a (CI) cloud band on the (equatorial) side of the jet stream.

25
Q

State the main explanation for the faster wind speeds at upper levels.

A

A lower density of the air.

26
Q

The greater the horizontal pressure gradient, the (closer/further apart) the isobars and the (stronger/weaker)​ the wind.

A

The greater the horizontal pressure gradient, the (closer) the isobars and the (stronger) the wind.

27
Q

Wind that has changed clockwise in direction can be said to have (backed/veered)​.

A

Wind that has changed clockwise in direction can be said to have (veered).

28
Q

In summer in the northern hemisphere, the maximum wind speeds associated with sub-tropical jet streams are usually located (below/above) the tropopause at about (100/200/250/300) ​hPa.

A

In summer in the northern hemisphere, the maximum wind speeds associated with sub-tropical jet streams are usually located (below) the tropopause at about (200) hPa ≈ 40.000 ft.

29
Q

Polar front jet streams over the South Pacific are usually strongest in (January/July)​.

A

Polar front jet streams over the South Pacific are usually strongest in (July).

- Strongest in Winter, which is in July on SH -

30
Q

Gradient wind speed (increases/decreases) with increasing latitude.

A

Gradient wind speed (decreases) with increasing latitude.

31
Q

On the Northern hemisphere over land, surface winds are (backing/veering) by about (…)° and speed slows down to about (…)​% of the 2000 ft geostrophic winds.

A

On the Northern hemisphere over land, surface winds are (backing) by about (30)° and speed slows down to about (50)% of the 2000 ft geostrophic winds.

32
Q

Cold anti-cyclones become (stronger/weaker)​ with height.

A

Cold anti-cyclones become (weaker) with height.