North American humid continental hot-summer climates are affected by conflicting maritime tropical (mT) and continental polar (cP) air masses.

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North American humid continental hot-summer climates are located in regions where maritime tropical (mT) air masses from the Gulf of Mexico and continental polar (cP) air masses from Canada meet, producing the characteristic climate of hot and humid summers, cold and snowy winters, and variable weather patterns throughout the year.

North American Humid Continental Hot-Summer Climates Are Affected by Conflicting