What is this in meteorology?

Air mass is a large volume of air defined mostly by uniform properties in temperature and humidity content. Air materials are categorized according to their temperatures and areas over which they gain their properties and play a major role in weather characteristics. Four main types of air mass are continental tropical, continental polar, nautical tropical and maritime polar. The air queue can also be categorized according to its stability in relation to the air below it. Warmer air mass tends to move towards colder areas and vice versa; When two materials meet, an air queue is formed. Tropical air mass contains warm air, while the polar mass of air contains cold air. The stability of air mass is also considered; Masses with colder air below them tend to be more stable than masses with a warmer air below them, because the mass tends to decline at altitude in view of these conditions. Meteorologists further categorize the air massE combination of humidity and stability conditions. Excellent air mass is dry and stable, while monsoon masses are humid and unstable.

air mass moves according to their temperature and density. The warm air moves towards the poles, while the radiator air moves towards the equator. In addition, dense air weights tend to be heavier and move down. This movement is responsible for various weather conditions and dictates the conditions of wind, temperature and humidity on the surface.

Movement also allows the formation of air fronts, points in which masses of different properties share the boundary. The dynamic movement caused by the difference in density, humidity and temperature in these areas is the cause of the weather of the weather to be typhoon and cyclones. Although wind shifts are a constant feature of air fronts, precipitation occurs only if there is sufficient humidity at the intersection. The air mass eventually movesThey rank far apart to eliminate the front and its resulting weather conditions.

In the formation of air fronts, several factors can affect. For example, volcanic eruptions can quickly heat the air in the area and increase the temperature of the air mass above it. The melting of the polar ice closures can also cause a significant increase in the humidity of the air mass above the head. At the same time, the weather conditions created by changing air queues and mass may affect the development of the masses that come afterwards.