Different air masses, such as mP and mT, contribute to the climate of regions like Florida. The collision of air masses plays a crucial role in storm development and weather patterns.
mP air masses are cool and moist, forming over oceans at approximately 60° N and S, while mT air masses are warm and moist, originating over oceans around 30° N and S. Maritime Tropical (mT) air masses affect the southeast and southwest U.S. coasts year-round, bringing warm and moist conditions. During cyclogenesis, the process of low pressure system formation, the interaction between different air masses leads to the development of storms and weather changes.
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