Cold, wet air.
The five types of air masses are polar, tropical, maritime, continental, and arctic. Polar air masses are cold and dry, tropical air masses are warm and dry, maritime air masses are warm and moist, continental air masses are dry and cold, and arctic air masses are extremely cold and dry.
Continental polar and continental tropical are alike in that they are dry air masses. The different between the two is that the continental polar is a cool air mass while the tropical is a very hot mass of air.
The 4 major air masses are continental polar (cP), continental tropical (cT), marine polar (mP) and marine tropical (mT). Generally, continental air masses are drier than marine air masses, and polar air masses are cooler than tropical air masses. cT air masses are relatively limited in distribution existing in the south west North America and North Africa.
Types of air masses that are characterized by their temperature and humidity characteristics. Continental polar and maritime polar air masses are cold and moist, while continental tropical and maritime tropical air masses are warm and humid. These air masses determine the weather conditions when they interact with each other.
yes
Continental air masses. Tropical air masses form over water.
the continental tropical and continental polar air masses both come from land, are humid and their differences are polar is cool air while tropical is warm air
Yes, tropical air masses tend to be warmer than polar air masses because they originate in regions closer to the equator where temperatures are higher. Polar air masses, on the other hand, come from regions closer to the poles where temperatures are colder.
polar continental
The 4 major air masses are continental polar (cP), continental tropical (cT), marine polar (mP) and marine tropical (mT). Generally, continental air masses are drier than marine air masses, and polar air masses are cooler than tropical air masses. cT air masses are relatively limited in distribution existing in the south west North America and North Africa.
Polar air masses develop over cold regions, primarily in the polar areas of the Earth, such as the Arctic and Antarctic. These air masses form when the surface temperature is significantly low, causing the air above to cool and become dense. As a result, polar air masses are characterized by cold temperatures and can influence weather patterns as they move towards lower latitudes.
Polar air masses form north of 50 degrees north latitude and south of 50 degrees south latitude. These air masses are characterized by their relatively cooler temperatures compared to tropical air masses.