Middle latitude cyclones are large centers of low pressure that generally travel from west to east and cause stormy weather.
Mid-latitude cyclones are typically comma-shaped.
A mid-latitude cyclone is a large scale area low pressure and cyclonically rotating air that occurs in the middle latitudes (i.e. neither tropical nor polar). Cyclonic rotation is defined as counterclockwise in the northern hemisphere and clockwise in the southern. Unlike tropical cyclones, such as hurricanes, mid-latitude cyclones are powered by temperature contrasts, usually along boundaries between large-scale air masses. These systems develop a system of fronts, usually with a warm front on the eastward side and a cold front on the equatorward side. These systems usually develop between 30 and 60 degrees of latitude.
Low pressure systems that cause stormy weatherweather
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Low pressure.
Mid-latitude cyclones are typically comma-shaped.
Mid latitude cyclones are typically comma-shaped.
Mid latitude cyclones are typically comma-shaped.
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Low pressure.
Mid-latitude cyclones are typically comma-shaped.
Mid-latitude cyclones are usually powered by temperature contrasts.
Mid latitude cyclones are typically comma-shaped.
Mid latitude cyclones are typically comma-shaped.
Middle-latitude cyclones (also called extratropical lows) often have a comma shape.
Middle-latitude cyclones (also called extratropical lows) often have a comma shape.
Pressure decreases toward the center
air high up in the atmosphere<-novanet
Pressure decreases toward the center
Convergent Counterclockwise