What is the inversion in meteorology?

Inversion is a situation where atmosphere layers do not normally, prevent normal weather processes and often capture smog, smoke and clouds near the ground. The most common form of inversion is temperature inversion, although inversion can have other forms. In essence, the inversion can be considered to be overturned in the natural order of things, suppressing a convection and other processes that allow air to cycle on the ground. When the temperature inversion occurs, the colder air is collected near the ground, with a layer of hot air pushing down on it. This forces clouds, smog and pollution to be trapped near the ground because they cannot go up and temperature inversions can sometimes break explosively, with heavy storms or tornadoes.

Inversion caused by cold air from the ocean surface that is pushing on the coast. Sea inversions explain why many coasts around the world are obscured. Inversion also commonly appears in valleys where warm air pushes into colder air in the valley. Because many urban areas are in the valleyEmi or near the ocean, often suffers from extreme pollution impaired by invers.

weather inversion does not only affect the weather in the area. Inversions can also affect human health, as in the case of inversion that captures pollution, and can also disrupt visibility by enforcing a heavy cloud cover near Earth. Inversions can also play funny tricks with radio signals and sounds; For example, radio signals are often stronger during inversion, and heavy fog characteristic of sea inversions can do special things to sounds, so they look further or close to than.

Inversion

will eventually be solved, sometimes quite suddenly, and sometimes appear and disappear several times during the day. In other cases, the inversion may apply for several days, which often leads to concerns about air quality and potentially dangerous weather conditions.

stop inversions in which a layer of hot air captureIt is a layer of colder air, they are notorious on the Midwest, because when the cap finally breaks, a huge amount of energy can be released, resulting in strong weather. The "cold" air in such inversions is often quite warm, so these inversions may feel very oppressed and tense until they finally disappear.