Midlatitude Cyclones
I. POLAR FRONT THEORY
A. Bjerknes
- frontal wave ("kink" in polar front) (animation)
- open wave = fully developed w/warm sector
- triple point -- secondary low
- energy source(s) for storm
- kinetic energy
- cold air sinks / warm air rises
- surface convergence = wind acceleration
- latent heat (of condensation)
- storm energy - tremendous!
B. Cyclogenesis
- definition:
development or strengthening of storms
- favored locations
- Rocky Mtns
- Gulf of Mexico
- Atlantic
- Great Basin
- keys
- divergence/convergence relationship
... second diagram
- divergence aloft
- lower density
- lower surface pressure
- = lift = storm
- convergence aloft
- higher density
- higher surface pressure
- = no lift = kills surface storm
- stacked vs. tilted storms
- stacked
- convergence aloft (no lift)
- subsidence
- kills surface storm
- tilted
- divergence aloft (lift)
- good "exhaust"
- lower level convergence
- storm movement
II. STORM TERMINOLOGY
A. Longwaves (Rossby Waves)
- troughs and ridges
- typically 4-6 in N hemisphere
- wavelength = 2400-5000 miles
- move ~4° long. per day
- seasonal drift north-south
B. Shortwaves
- disturbance embedded in longwave
- faster movement
- approx. speed of 700mb flow
- can deepen longwave trough and strengthen themselves
C. Retrograde
D. General Terminology
- barotropic conditions
- height contours parallel isotherms
- baroclinic conditions
- pressure contours cross isotherms
- cold / warm advection
= increase in temperature contrast
= strengthens storm
- baroclinic = instability
- cut-off low
vs. closed low & split flow
- comma clouds
... another example
- jet maximum or jet streak
= upper divergence
E. Vorticity
- related to divergence aloft (see I.B.4. above)
- strong divergence aloft = strong updrafts
- = increases spin = surface vorticity
- positive vorticity
- cyclonic (counterclockwise)
- planetary vorticity
- vorticity due to spin of earth
- min = equator; max = poles
- relative vorticity
- curvature of flow + diff. wind speeds
- diff. in speed = shear = vorticity
- absolute vorticity = planetary + relative
- "vort max"