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A tropical cyclone is characterized by organized convection and thunderstorms. This convection, fueled by warm, moist air, is what powers a tropical cyclone. Because of the amount of moisture needed, these systems can only develop over warm ocean water. Because of their tropical origin, tropical cyclones usually form in environments of relatively little temperature contrast. The core of a tropical cyclone is generally warmer than its surroundings.

A temperate cyclone, more often called and extratropical or mid-latitude cyclone usually lacks organized convection. When convection does occur with these systems, it usually does not play a key role in the system's development. They are powered by collisions between warm and cold air masses, and so form in areas of large temperature contrasts. Unlike their tropical counterparts, these systems tend to be strongest in cold environments.

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Tyrese Nolan

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