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A cP (continental polar) air mass is generally cool and dry.
Air formed in places where the temperature is warm.
continental polar
Continental polar masses are cold and dry air masses because the cold air cannot hold much moisture. As they move into warmer air, they can trigger precipitation.
An air mass is a body of air. It has similar characteristics to the land on top of which it forms. Fronts are the boundaries in between two different, or same air masses. (e.g: a cold front is when a cold air mass hits a warm air mass and quickly pushes the warm air mass upward.)
The continental tropical air mass is very humid and warm, with lots of rain and a high humidity.
A cP (continental polar) air mass is generally cool and dry.
Air formed in places where the temperature is warm.
dry
continental tropical
Warm, humid
it is continental tropical air
A warm and dry air mass can make the area over which it moves arid and less humid. This is why deserts have dry air while coastal areas are humid.
dry and warm
The boundaries between air masses are called front. The types of air mass and movements involved determine the type of front. Warm front: a warm air mass plows into a cold air mass. Cold front: a cold air mass plows into a warm air mass. Stationary front: The warm and cold air masses move little relative to one another. Occluded front: A cold front catches up with a warm front, sending the warm air mass aloft. Dry line: a dry air mass plows into a moist air mass.
A warm dry air mass typically brings clear skies, warm temperatures, and low humidity to the area over which it moves. It can lead to dry conditions and increased evaporation, which may contribute to heatwaves and drought.
yes