Fronts and Mid latitude cyclones Flashcards

1
Q

What is a front

A

a boundary between two different air masses

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

how wide are fronts

A

100-200km wide

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

are transitions over fronts sharp and abrupt

A

yes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Where do fronts mainly occur

A

mid latitudes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

what type of pressure are fronts associated with

A

low pressure systems

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

In a warm front what air is where

A

warm air flows up over dense air

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

how much is the inclination of this frontal surface

A

0.5-1

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

what (cloud) signals the approach of a warm front

A

high cirrus or cirrostratus clouds with the cloud base lowering as the front approaches

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

what rain occurs at the warm front

A

rain starts ahead of the surface front and is widespread and persistent

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

what happens after the passing of a warm front

A

skies clear quickly

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

explain what happens with a cold front (1)

A
  • dense cold air pushes forward into the warmer air which is forced upwards
  • this forms deep convective clouds above the surface front with heavy rain along this band
  • behind the front the cloud base lifts, eventually clearing
  • near the surface the cold air may surge forward, producing a very steep frontal zone
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

explain what happens with a cold front (2)

A
  • Dense cold air pushes forward into warmer air, and over-runs it.
  • Deep convective clouds form ahead of upper front, heavy rain in narrow band along upper front
  • Between upper and surface fronts, there is shallower cloud.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Explain what happens at a stationary front

A

There is only a small difference between the air masses either side of the stationary front – the front is defined by the direction of motion only
When the boundary between air masses does not move it is called a stationary front
Note that the wind speed is not zero – the individual air masses still move, but the boundary between them does not

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Explain what happens at an occluded front

A

In general cold fronts move faster than warm fronts, and may thus catch up with a warm front ahead – the result is an occluded front
There are two types of occluded fronts: warm and cold, depending on whether the air behind the cold front is warmer or cooler than the air ahead of the warm front
Warm occlusions are the more common type in the UK
Occlusion is part of the cycle of frontal development and decay within mid-latitude low pressure systems

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

explain what happens at a warm occlusion

A

In both warm and cold occlusions, the wedge of warm air is associated with layered clouds, and frequently with precipitation
Precipitation can be heavy if warm moist air is forced up rapidly by the occlusion

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Explain a cold occlusion

A

Regarded to be very rare. Some believe that they do not exist

17
Q

what is a mid-latitude cyclone

A

Low pressure systems (or mid-latitude cyclones) are a characteristic feature of mid-latitude temperate zones

18
Q

What happens with a mid-latitude cyclone

A

Low pressure systems form in well defined zones associated with the polar front
Provide a strong temperature gradient and convergent flow resulting from the global circulation

19
Q

Explain the Norwegian cyclone model

A

-Low pressure forms at surface over “polar front” due to divergence aloft
-As rotation around initial low starts, a ‘wave’ develops on the polar front
-Flow near surface is directed towards the low centre due to friction
-Mass balance: inward flow compensated by large-scale lifting cooling  cloud formation
-Surface low is maintained (or deepens) due to divergence aloft exceeding convergence at surface
-Cold sector air pushes cold front forward; warm sector air flows up warm front – warm front moves slower than cold
-Cold front overtakes warm front to form an occlusion, which works out from centre
-Depression usually achieves maximum intensity 12-24 hours after the start of occlusion
-Low starts to weaken as inflowing air ‘fills up’ the low pressure
Low continues to weaken, clouds break up

20
Q

what is a conveyor belt

A

belts of low wind levels identified ahead of cold and warm fronts

21
Q

explain the warm conveyer belt at the cold front

A
  • Main source of warm, moist air that feeds the cyclone
  • Originates in the warm sector of the cyclone
  • Air ascends as it approaches the cyclone
22
Q

explain a cold conveyer belt at a warm front

A
  • Originates on the poleward side of the warm front

- Air becomes saturated through ascent and rain falling from WCB above

23
Q

Crossed-winds rule: if the upper wind from your LEFT

A

the weather is likely to deteriorate

24
Q

Crossed-winds rule: if the upper wind from your RIGHT

A

the weather is likely to improve

25
Q

crossed-winds rule: if the upper wind is BEHIND or AHEAD of you

A

there is likely to be a little change in the weather