Fronts Flashcards
What is a front
A place where air masses meet
Developing front symbol
Triangles with dots
Could also be called frontal-genesis
Decaying front symbol
Triangles with crosses
Could also be called frontolysis
Quasi front
Stationary front
Little movement, 5 kts
Caused by parallel isobars and geostrophic wind running parallel to the front
Very unstable
Doesn’t last very long
Polar front
Marks the boundary between polar maritime and tropical maritime air masses
Boundary between polar and Ferrell cells
Varies due to seasons and land masses
Average position is 50*N/S
Intertropical front
ITCZ
Zone of converging air-masses due to trade winds
Mediterranean front
Only in winter
Warm winds from the south meet colder winds from the European land mass
Arctic front
Only forms in winter, the temp is so low that a pressure gradient is formed
Can be very faint
Can create an arctic front jet stream
N America/america
Frontal surface
Slopping boundary between air masses
Approx 3-5km long
Summer polar front
Canada to over Scotland
Around 65* max north
Winter time polar front
Florida to SW uk
Can be as low as 35* max
Polar front depression
A low is created off the coast of Florida which could be caused by high winds.
The cold air undercuts the air, making the waves bigger down the front
Other names for PFD
Westerly waves
Frontal waves
Westerly situation
Speed of the fronts in a PFD
Cold, same speed as system
Warm, 2/3rds of the speed
To establish the speed and direction of a PFD
Use the first 2 isobars
The direction they are pointing is the direction the front is moving
The spacing between 2 isobars is the speed