Chapter 18: Meteorology: Fronts & Frontal Depressions Flashcards
Creation / Destruction of Front
Frontogenesis -> converging masses
Frontolysis -> diverging masses
Front Neutral Surface
What is? Characteristics (2)?
Where two fronts meet
Ground: 100 nmi
Depth: 5000 - 6000’
Fronts
Front Types Around UK (3), Which one is all year round? Where is its frontal line?
Artic Front (W) Mediterranean Front (W) Polar Front (S+W) Summer: Nova Scotia to Scotland Winter: Florida to SW UK
Polar Front Depression Formation
Formation
- Quasi-stationary front: polair air N, tropical air S
- Warm air above cold air -> depression
- NH: CCrot -> brings warm front in front, cold behind
Polar Front Jet Location
Why can there be confusions?
On map: in cold air
In reality: in warm air
because map doesn’t take into account slant of fronts
Warm Front
Length, gradient, windspeed
500 nmi
1:150 - 1:180 gradient
V = 2/3 Vwind @ 3000’ = 10 kn
Cold Front
Length, gradient, windspeed
300 nmi
1:50 - 1:80
V = Vwind @ 3000’ = 15kn
Polar Front Warm Air (Middle Section)
What Cloud, vis to expect with MT? CT?
MT: Summer: Fair weather Cu, 5km vis Winter: St, FG, Sc, < 5km vis CT: Better vis, SKC
Polar Front Depression Movement (2)
V, how long does PFD travel over a place?
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
Wind Change (NH) Through PFD, north of PFD, at warmF into Jetstream, at coldF into jetstream
Veering
Backing
Veering
Backing
Secondary Low
Under coldF, second depression
Temporary Cold Anticyclones
On both sides of PFD, cold anticyclones
Occlusions
Warm/cold front meet and close up PFD Cold occ (S): coldest air behind Warm occ (W): coldest air in front