Extratropical cyclones are low-pressure systems that form outside of the tropics in response to chronic instability of the westerly winds. Because this instability is dependent on large horizontal temperature contrasts, concentrated regions of temperature change known as fronts characterize extratropical cyclones.
These storms populate the middle and high latitudes, north of 35 degrees latitude in the Northern Hemisphere, and thus they also are called “mid-latitude cyclones.” If the barometric pressure of a mid-latitude cyclone falls by at least 1 millibar per hour for 24 hours, the storm is referred to as a “bomb cyclone.”
A tornado is a rapidly rotating column of air extending downward from a thunderstorm to the ground. The most violent tornadoes are capable of tremendous destruction with wind speeds of up to 300 mph.
Tornadoes form in regions of the atmosphere that have abundant warm and moist air near the surface with drier air above, and a change in wind speed and wind direction with height above the ground.