Maritime by definition is humid.
Maritime polar and tropical, continental polar and tropical.
dry
Warm, humid
Maritime polar air masses bring cool and humid weather. These air masses originate over cold ocean waters and bring moisture with them, leading to cooler and more humid conditions as they move over land.
Air masses with those characteristics are termed "maritime tropical".
Maritime polar and tropical, continental polar and tropical.
dry
The maritime tropical air mass is warm and humid.
Warm, humid
It is humid.
Warm, humid
Warm, humid
The four general air mass classifications are maritime tropical (mT), continental tropical (cT), maritime polar (mP), and continental polar (cP). Maritime tropical air masses are warm and humid, originating over oceans in tropical regions. Continental tropical air masses are hot and dry, forming over land in warm regions. Maritime polar air masses are cool and moist, while continental polar air masses are cold and dry, both originating in higher latitudes.
Maritime polar air masses bring cool and humid weather. These air masses originate over cold ocean waters and bring moisture with them, leading to cooler and more humid conditions as they move over land.
Air masses with those characteristics are termed "maritime tropical".
Air masses are classified based on their source regions, and the main types include continental polar (cP), maritime polar (mP), continental tropical (cT), and maritime tropical (mT). Continental polar air is cold and dry, originating from land areas in high latitudes. Maritime tropical air is warm and humid, coming from ocean regions in warmer latitudes. Continental tropical air is hot and dry, while maritime polar air is cool and moist, both originating from their respective land and ocean locations.
Maritime tropical (mT) air masses originate over warm ocean waters in tropical regions, bringing humid and warm conditions. Maritime polar (mP) air masses form over cold ocean waters in polar regions, resulting in cool and damp weather. Continental tropical (cT) air masses develop over hot, dry land areas, leading to warm and dry conditions. Continental polar (cP) air masses arise over cold land areas in polar regions, producing cold and dry air.