One characteristic of mid-latitude cyclones that other types of cyclones do not have is a frontal boundary. Mid-latitude cyclones, also known as extratropical cyclones or low-pressure systems, are typically associated with the convergence of warm and cold air masses. This results in the formation of a frontal boundary, where warm air rises over the colder air, leading to the development of clouds, precipitation, and atmospheric disturbances. In contrast, tropical cyclones, such as hurricanes or typhoons, do not have a distinct frontal boundary as they are fueled primarily by warm ocean waters.
