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An air mass
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.
An air mass is a large body of air that has relatively uniform temperature and humidity characteristics. The regions where air masses form are referred to as air mass source regions. If air remains over a source region long enough, it will acquire the properties of the surface below. Ideal source regions are regions that are generally flat and of uniform composition. Examples include central Canada, Siberia, the northern and southern oceans and large deserts.
Air masses get properties of the surface beneath them from areas known as source regions. Individual regions span several million square miles in size.
It separates hot air masses and cold air masses
Temperature and moisture
An air mass
It is an air mass.
When one air mass bump into one another, the air masses usually doe not mix because the properties of the air masses are different. A front forms between the two air masses. Stormy weather often occurs along fronts.
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.
An air mass is a large body of air that has relatively uniform temperature and humidity characteristics. The regions where air masses form are referred to as air mass source regions. If air remains over a source region long enough, it will acquire the properties of the surface below. Ideal source regions are regions that are generally flat and of uniform composition. Examples include central Canada, Siberia, the northern and southern oceans and large deserts.
In addition to their overall temperature air masses are classified according to the surface over which they form. continental air masses form over land, and are likely to be dry. Maritime air masses form over water and are humid. Polar air masses form at high altitudes and are cold. Tropical air masses form at low latitudes and are warm
Air masses get properties of the surface beneath them from areas known as source regions. Individual regions span several million square miles in size.
A front, or boundary between two air masses, is typically characterized by clouds and precipitation. The amount and type of precipitation typically depends on the temperature and moisture difference between the two air masses. Generally speaking, stronger temperature/moisture differences mean more clouds and precipitation.
There are two types of air masses: COLD AIR AND WARM AIR.Cold Air Masses-Cold air masses can cause thunderstorms and even tornadoes.Warm Air Masses-Warm air masses can bring many hours of steady rain and snow.
true??
maritime and continental.