Polar Front Theory - Development and Evolution of a Wave Cyclone, Cont.

(c)- A fully-developed "wave cyclone" is seen 12-24 hours from its inception. It consists of:

  • a warm front moving to the northeast
  • a cold front moving to the southeast
  • region between warm and cold fronts is the "warm sector"
  • the central low pressure (low, which is deepening with time)
  • overrunning of warm air over the warm front
  • cold air surging southward behind the cold front
  • wide-spread precip ahead of the warm front
  • narrow band of precip along the cold front
  • Wind speeds continue to get stronger as the low deepens - the Available Potential Energy (APE)is being converted to Kinetic Energy (KE)
  • The production of clouds and precip also generates energy for the storm as Latent Heat is released
image adopted from Understanding Weather and Climate by Aguado and Burt, © 1999 by Prentice-Hall, Inc