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dry continental air masses.
southwest monsson
Continental Tropical air masses (cT) A continental tropical air mass forms in the interior of subtropical continents at about 15o to 35o north and south latitude. They are hot and dry air masses due to the temperature and moisture characteristics at their source region.
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.
Continental air masses. Tropical air masses form over water.
dry continental air masses.
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.
Dry continental air masses. Much of the land is desert with a dry, hot climate.
southwest monsson
because continental air mass forms over land so it is dry
Continental Tropical air masses (cT) A continental tropical air mass forms in the interior of subtropical continents at about 15o to 35o north and south latitude. They are hot and dry air masses due to the temperature and moisture characteristics at their source region.
Dry continental air masses. Much of the land is desert with a dry, hot climate.
cold and dry
cold air sinks as denser - warm air rises
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.
Continental air masses. Tropical air masses form over water.
warm and hummid, cool and huimid, warm and dry, cool and dry