Mid-latitude cyclones Flashcards
Other names for mid-latitude cyclones
frontal depression, extratropical cyclone, temperate cyclone
Origin:
forms at 60 degree N & S latitude at polar front, where warm air from subtropics meets cold air from poles.
Circulation:
in S hemisphere, air moves clockwise into centre of LP pressure system - converges and rises.
Diameter
1000-4000 km wide
Movement
in Rossby waves (help transfer heat from the tropics toward the poles and cold air toward the tropics in an attempt to return atmosphere to balance) from West to East within westerly wind belt (30 -60 latitude); travel at speeds of 40 - 90 km/h.
Season
all year round, but mostly influence our weather in winter when CF bring rain to SW cape. In Summer, they migrate south with shifting of sun’s rays and little effect on SA weather.
Duration
2-5 days, but can last up to 14 days
Where is the worst weather experienced within the cyclone?
closest to centre of LP
Stages in formation of mid-latitude cyclone (cyclogenesis):
1st stage
Initial/developing/wave stage:
forms at polar front; warm, moist sub-tropical air meets cold, dry polar air.
2 air masses move in opposite directions (don’t mix)
the disturbance, due to rotary movement, causes LP to form at wavepoint.
Stages in formation of mid-latitude cyclone (cyclogenesis):
last stage
Mature (warm sector) stage:
cold & warm fronts develop. Air circulates clockwise around and into the low pressure and rises.
warm front: warm air rises gradually over cold air ahead of it.
cold front: cold air wedges in under warm air, forcing it to rise sharply.