The source region of an air mass defines its main characteristics.
The temperature of an air mass will depend largely on its point of origin and its subsequent journey over the land or sea. This might lead to warming or cooling by the prolonged contact with a warm or cool surface.
A warm air mass is produced by prolonged contact with a warm surface, and conversely a cold air mass is produced by prolonged contact with a warm surface. The heat transfer processes that warm or cool the air take place slowly. It may take a week or more to warm up the air by 10 oC right through the atmosphere, and in order for these changes to take place a large mass of air must stagnate over a region. Parts of the earth's surface where the air can stagnate and gradually gain properties of the underlying surface are called source regions.
The main source regions are the high pressure belts in the sub tropics (giving rise to tropical air masses) and around the poles (the source for polar air masses).
Warm source regions (tropical air masses):
Cold source regions (polar air masses):
Last updated: 14 August 2013