In this cyclone model, when warm air from the Equator and cold air from the Southern Hemisphere collides, it moves clockwise. On the other hand, when warm air from the Equator and cold air from the Northern Hemisphere collides, it adopts a counter-clockwise direction. The main difference here is the direction of the wind. Secondly, the cold and warm fronts are different. For instance, in the first model (warm air from Equator and cold air from South Hemisphere), the cold front tends to be in the easterly while in the other model, the cold front is likely to be westerly. However, in both models, the consequences of the cyclones are similar; clouds will form, resulting in different types of precipitation such as rainfall and snow fall (Pidwirny, 2006). Secondly, in both models, winds tend to blow towards the easterly direction; that is both the clockwise and counter-clockwise movements make the winds to blow to the east.
The continental Arctic type of air mass moving from the Southern Hemisphere towards the Equator will move in a clockwise direction, which means it will adopt a westerly direction. Therefore, areas in the western part will be affected by the cold Arctic air mass. On the other hand, an arctic air mass moving from the Northern Hemisphere towards the Equator will adopt a counterclockwise movement or direction. That means areas to the East of the Northern Hemisphere towards the Equator will experience the effects of the Arctic air mass, which is much colder, but will eventually warm up at the Equator.
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Reference
Pidwirny, M. (2006). "The Mid-Latitude Cyclone". Fundamentals of Physical Geography, 2nd Edition . http://www.physicalgeography.net/fundamentals/7s.html
