chapter 7: Jet and Jet streaks Flashcards

1
Q

Weather processes strongly depend on

A

the structure and dynamics of jet streams

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2
Q

There are ………………….major ……………………jet streams in the upper ………………………in each hemisphere

A

two

westerly

troposphere

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3
Q

There are two major westerly jet streams in the upper troposphere in each hemisphere

A

– Polar jet stream
– Subtropical jet stream

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4
Q

The structure of jet streams are related to

A

temperature distribution through the thermal wind relationship

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5
Q

Warm air to the south results in

A

westerly geostrophic winds through the thermal wind relationship.

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6
Q

Draw the jet stream (box)

A
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7
Q

The thermal wind relationship also explains why

A

the jet stream tends to be collocated with the polar front.

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8
Q

Large horizontal temperature gradients > > >

A

large horizontal temperature gradients

Large thickness gradients>

Large horizontal pressure gradient aloft>

strong winds

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9
Q

The polar jet is the band of

(speed ) (found in)

A

meandering strong winds (~100 knots) found at the tropopause.

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10
Q

The polar jet moves

A

meridionally (30°-60° latitude) and vertically (10-15 km) with the seasons.

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11
Q

Large vertical extent: maximum usually near ……………….. but can be seen at ……………….

A

300 mb

200mb - 500mb

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12
Q

At times, the polar jet will split into …………………………….and possibly merge with ………………………..

A

northern and southern branches

the subtropical jet

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13
Q

Polar Jet and thermal wind balance:

it is associated with:

A

strong quasi-horizontal temperature gradients in the lower troposphere and strong vertical wind shear.

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14
Q

It is associated with strong quasi-horizontal temperature gradients in the lower troposphere and strong vertical wind shear.

• These features are often associated with

A

the polar front.

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15
Q

Meridional undulations of the jet stream are associated with

A

poleward and equatorward displacements of warm and cold air, respectively.

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16
Q

The subtropical jet is associated with……………………………………. between……………………… usually found between…………………….

A

subtropical front between the tropical and mid-latitude air masses and is usually found between 25° and 30° N.

17
Q

It meanders less than…………………………., but in rare cases has been observed as far…………………………

A

the polar jet

north as 60°N

18
Q

Subtropical jet is ………………………

A

shallow

19
Q

subtropical jet stream is rather shallow – sometimes less than ……………………………..and may not show up on……………………………..

A

3 km in depth

either of the 200 mb or 300 mb standard levels

20
Q

Subtropical Jet Stream directly influences …………………………..

A

low-level flow only when it becomes coupled through deep cumulus convection and interactions with the polar jet

21
Q

what are the two cases that subtropical jet streams affect low:

A
  1. when it becomes coupled through deep cumulus convection and
  2. interactions with the polar jet
22
Q

Like the Polar-Front jet, the subtropical jet is associated with a

A

change in height of the tropopause.

23
Q

The meridional temperature gradient associated with the

A

vertical shear under the subtropical jet is concentrated in a shallow layer

24
Q

Sometimes the subtropical jet is associated with a

A

a portion of the Polar-Front jet that has migrated equatorward into the subtropics and has lost its low-level baroclinicity.

25
Q

define Barcoclinicity

A

surfaces of pressure intercect surfaces of temperature and density (occure at fronts)

FRONT HAS BAROCLINITY

26
Q

Subtropical Jet position is …………….. than polar jet

A

higher

27
Q

subtropical jets and polar jet separate ……..

A

cells

28
Q

The presence of the subtropical jet relates to the

A

conservation of absolute angular momentum in the context of the Hadley cell.

29
Q
A