
большие объемы воздуха тропосферы обладающие однородными свойствами и влияющие на формирование
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The term for large volumes of air in the troposphere with homogeneous properties that influence climate is air masses.
Air masses are large bodies of air that have similar temperature, humidity, and stability characteristics throughout. They can cover vast areas and can persist for several days or even weeks. Air masses play a crucial role in shaping weather patterns and climate conditions in different regions.
Air masses are classified based on their source regions and the characteristics they acquire while traveling over different surfaces. The five primary air mass classifications are:
1. Continental Polar (cP): These air masses form over cold land areas and are characterized by low temperatures and low moisture content. When they move over warmer regions, they can bring cold and dry conditions.
2. Continental Tropical (cT): These air masses originate from hot and dry regions, such as deserts. They are associated with high temperatures and low humidity. When they move into other areas, they can bring hot and dry conditions.
3. Maritime Polar (mP): These air masses form over cold oceanic regions and are characterized by cool temperatures and high moisture content. When they move over land, they can bring cool and moist conditions.
4. Maritime Tropical (mT): These air masses originate from warm oceanic regions and are associated with warm temperatures and high humidity. When they move over land, they can bring warm and humid conditions.
5. Arctic (A): These air masses form over the Arctic region and are extremely cold. They are not as common as the other air masses and usually stay confined to high latitudes.
The interaction of different air masses can lead to the formation of weather systems, such as fronts, which can result in changes in temperature, precipitation, and wind patterns.


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