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If the observer is only a short distance south of the low-pressure centre, then the cold front would follow rapidly.
The cold front itself usually contains strong winds, and is often preceded by a squall line containing truly dangerous winds.
The horizontal gradient of the buoyancy term always tends to propagate the cold front.
In their studies they assumed that the flow in the cold front was motionless relative to the moving front.
The direction remained fairly constant until it veered to around 220x when the cold front went through around 1323 hours.
Here a curved warm front on the eastern side meets a curved cold front that follows it.
The atmospheric pressure rises as the cold front passes.
As the core of the cyclone passes, the cold front of a high-pressure zone follows, generally accompanied by a squall line that brings violent and destructive winds.
A slow-moving cold front covered much of the operational area, giving conditions of dense cloud from 700 feet to 15,000 feet.
Where is the warm front and where is the cold front?
After maintaining peak winds for about 18 hours, the storm rapidly weakened, as it interacted with an approaching cold front.
Its associated cold front traversed much of the outbreak affected area with several supercells forming ahead of front.
Winds ahead of an approaching cold front or low pressure system can also draw the marine layer onshore.
The fast moving cold front pushed a storm through the city rather quickly, dumping 0.81 inches of rainfall in a relatively short time.
Maintaining hurricane status for about 18 hours, the storm continued rapidly northeastward and weakened due to strong wind shear from the approaching cold front.
