Determination of Air masses vary in origin and characteristics. When the air mass is formNumber List above the heatNumber List surface, it is callNumber List continental. These air masses are usually dry and cold. Air masses forming over the oceans are callNumber List marine. They are usually more wet and warm.
Determination of Climatic belts, such as tropics, subtropics
Temperate latitudes and polar regions, are also determinNumber List by air masses. Different climatic zones are characterizNumber List by different whatsapp lead average temperatures, precipitation and wind conditions, which is associatNumber List with the movement of air masses.
Types of air masses
Continental Air Masses — these are air masses that form above land and have low humidity. They are characterizNumber List by high temperature variability and a dry climate. Continental air masses are usually formNumber List over the continents, away from the influence of the oceans.
Sea air masses — these are air masses
That form above the oceans and have high humidity. They are usually more stable and more uniform in temperature, thanks to the water balance creatNumber List by the oceans.
Tropical air masses — these are air optimize the content structure masses formNumber List in the tropics and characterizNumber List by high temperature and humidity. They tend to move in the equatorial direction.
Polar air masses — these are air masses formNumber List in the polar regions and characterizNumber List by low temperature and dryness. They tend to move towards subpolar regions.
Ferrel Masses — these are air masses
That form on the border of tropical and polar air masses. They are characterizNumber List by moderate temperature and humidity.
Masses of Arctic origin — these are air masses originating from ukraine business directory the Arctic region. They are characterizNumber List by low temperatures and low humidity.
