Chapter 18: Meteorology: Fronts & Frontal Depressions Flashcards

1
Q

Creation / Destruction of Front

A

Frontogenesis -> converging masses

Frontolysis -> diverging masses

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2
Q

Front Neutral Surface

What is? Characteristics (2)?

A

Where two fronts meet
Ground: 100 nmi
Depth: 5000 - 6000’

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3
Q

Fronts

Front Types Around UK (3), Which one is all year round? Where is its frontal line?

A
Artic Front (W)
Mediterranean Front (W)
Polar Front (S+W)
Summer: Nova Scotia to Scotland
Winter: Florida to SW UK
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4
Q

Polar Front Depression Formation

Formation

A
  1. Quasi-stationary front: polair air N, tropical air S
  2. Warm air above cold air -> depression
  3. NH: CCrot -> brings warm front in front, cold behind
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5
Q

Polar Front Jet Location

Why can there be confusions?

A

On map: in cold air
In reality: in warm air
because map doesn’t take into account slant of fronts

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6
Q

Warm Front

Length, gradient, windspeed

A

500 nmi
1:150 - 1:180 gradient
V = 2/3 Vwind @ 3000’ = 10 kn

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7
Q

Cold Front

Length, gradient, windspeed

A

300 nmi
1:50 - 1:80
V = Vwind @ 3000’ = 15kn

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8
Q

Polar Front Warm Air (Middle Section)

What Cloud, vis to expect with MT? CT?

A
MT: 
Summer: Fair weather Cu, 5km vis
Winter: St, FG, Sc, < 5km vis
CT: 
Better vis, SKC
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9
Q

Polar Front Depression Movement (2)

V, how long does PFD travel over a place?

A

V = 80% Vwind @ 3000’ = 12kn
Passage of PFD = 9 - 12h

Straight along isobar between cold and warm front
Warm/cold front spreads and gets bigger

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10
Q
Wind Change (NH)
Through PFD, north of PFD, at warmF into Jetstream, at coldF into jetstream
A

Veering
Backing
Veering
Backing

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11
Q

Secondary Low

A

Under coldF, second depression

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12
Q

Temporary Cold Anticyclones

A

On both sides of PFD, cold anticyclones

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13
Q

Occlusions

A
Warm/cold front meet and close up PFD
Cold occ (S): coldest air behind
Warm occ (W): coldest air in front
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