Continental tropical air masses are most prominent in the desert Southwest of North America, the high plains, and northern Mexico in relation to the United States.
These are hot and extremely dehydrated and they usually develop during summer. The air has quite soft dew points and is warm to sizzling afternoon temperatures but with benign night-time temperatures.
The warm temperate zone rises on the southeast coasts of the United States to the Mississippi River and over the Gulf Coast; the zone is extremely impacted by the warm, humid tropical air mass that arises over the Gulf of Mexico.
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