Jet Stream Flashcards

1
Q

Width of jet stream =
Length=
(Minimums)

A

200NM

2000NM

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2
Q

Low pressure around equator because

A

Hot air rising more. (Bc of positioning to sun, the tilt). As hot air rising, low pressure is left at the bottom

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3
Q

Higher pressure in colder areas as

A

Hot air rises, but bc it’s dense it doesn’t leave a void of low pressure. Air comes back down after rising, compresses, causes high pressure.

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4
Q

Troughs represent

A

Pressure decrease, like a trench downwards.

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5
Q

Orographic Low/depressions

A

Mountains, ALPS eg. Air moves around mountains, meaning area behind mountains have low pressure.

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6
Q

High pressure systems

A

Air moves down, gets warmer

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7
Q

Small scale heat

A

Ground heat moves up to tropopause

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8
Q

Large scale heat

A

Earths tilt, heating dependant on that

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9
Q

Ride of high pressure

A

Extension of high pressure regions. Protrude outwards into other pressure regions

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10
Q

Anticyclones =

A

High pressure.

In N Hemisphere, spin clockwise

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11
Q

Cyclones in northern hemisphere

A

LOW pressure

Wind spins anti clockwise

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12
Q

Buy ballots law

A

Back to wind in northern hemisphere. Low pressure to the left.

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13
Q

Blocking anticyclones

50⚫️N and 70⚫️N

A

Block depression (low pressure) movement

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14
Q

COL

A

Saddle shaped ridge. Between two highs or two lows

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15
Q

In day, around 2/3pm sea breeze…

A

Comes across from sea to land. Highest amount of air has risen from land. Greatest temperatures. Leaves greatest low pressure at bottom. For high pressure cold sea breeze to fill

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16
Q

At night time. Sea has high specific heat capacity. So hot air only rises significantly at night, causing low pressure. This means that breeze come from

A

Land over sea. Pressure is now higher over land, as the land has cooled.

17
Q

Anabatic wind

A

DAYTIME

Hot air rises up the sides of the mountains.

18
Q

Katabatic wind

A

NIGHT TIME.

cold, heavy air, flows down into valley, gets lower, and gets colder, gets denser.

19
Q

The Bora (katabatic)

A

Cold air found around coastlines east of Adriatic sea. Cold air comes down from alps and from east Croatia.

20
Q

Jet streams tend to flow

A

From west to east

21
Q

The mistral

A

Airflow between two mountains. Like Venturi. Area decreases, speed increases.
Happens around southern France area. Goes into the Mediterranean.

22
Q

Fohn wind

A

Air approaches mountain. Rises, cools. Use DALR 3⚫️ per 1000ft. Humidity increases, eventually reaches 100% saturation. Then use SALR 1.8⚫️ per 1000ft. In which case clouds are formed. Will then precipitate, as can’t hold any more water. Then eventually moves back to DALR as it heats back up again when coming down other side of mountain.

23
Q

African winds (local winds) going into Mediterranean

A

Sirocco
(north west)

Ghibli
(central Northern Africa)

Khamsin
(towards Egypt area, going into Mediterranean)

24
Q

Global surface winds

Refer to picture in gallery (of globe with many arrows on. And roaring something bottom right of page.

A

Hadley cells above and below ITCZ.
Ferrell cell after Hadley
Polar cells after Ferrell

25
Q

ITCZ

A

Inter tropical convergence Zone