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Both temperate and tropical cyclones are low pressure adiabatic systems. However, the temperate cyclones are those which occur in mid latitudes i.e. 400 to 600 N & S. These are formed due to convergence of the warm (tropical) and Cold (Polar) airmasses. This is important to note that there confusion somewhere that these are formed by the convergence of warm and cold winds. Difference between winds and airmasses should carefully be understood. These cyclones, being convergence of contrasting airmasses, have clear and well developed fronts. In this way the entire cyclones is divided into four regions /parts. 1. Warm sector; 2. Cold sector; 3. Warm front; and 4. Cold front. The isobars of temperate cyclones are Wedge shaped or oval shaped. Whereas the tropical cyclones are those which occur in lower latitudes, normally 100 to 300 N & S latitudes and are caused due to the convergence of warm dry and warm moist airmasses. These cyclones do not experience fronts, or if have, then very weak fronts. The weather conditions, associated with the cyclone, are studied on the following 5 bases. 1. before arrival of cyclone; 2. Arrival of fore part; 3. Eye of the cyclone; 4. Arrival of back part; and 5. After departure of the cyclone. The isobars of tropical cyclones are circular.

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15y ago
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11y ago

temperate cyclones or extra tropical cyclones are most dominant over the north Atlantic Ocean, especially during winter. they are much larger in diameter than that of tropical cyclones, but possess weaker pressure gradient.

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11y ago

Tropical monsoons are the monsoons in tropical zone i.e. near the equator.

Temperate monsoons are the monsoons in temperate zone where climate is moderate. Tropical monsoons are quite hot than the temperate. Tropical monsoons regions are comparatively developed than temperate.

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Q: Temperate and tropical cyclones
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