Influence of inversion temperature

Inversion refers to the phenomenon that atmospheric temperature increases with height. The influence of inversion is mainly reflected in the following aspects: 1. Stability of atmospheric stratification: the existence of inversion layer makes atmospheric stratification more stable and hinders the vertical movement of air. This will lead to the accumulation of air pollutants under the inversion layer, which is difficult to spread and dilute, thus aggravating the degree of air pollution.

2. Uneven temperature distribution: The existence of inversion layer leads to uneven vertical temperature distribution. The ground temperature below the inversion layer is low, and the temperature above the inversion layer is high. This uneven temperature distribution will affect the stability of the atmosphere and the formation of wind, and then affect the changes of meteorology and climate.

3. Reduced visibility: Water vapor and particulate matter are easy to accumulate in the air below the inversion layer, which increases the air humidity, thus reducing visibility. The inversion layer will also lead to weather phenomena such as fog and haze, further affecting visibility.

4. Affect the growth of crops: The existence of inversion layer will reduce the ground temperature, especially at night, which may adversely affect the growth of crops. The ground temperature below the inversion layer is low, which is easy to cause climate disasters such as frost and damage crops.

In a word, the influence of inversion is mainly reflected in the stability of atmospheric stratification, uneven temperature distribution, reduced visibility and the impact on crop growth.