advection radiation fog

简明释义

平流辐射雾

英英释义

例句

1.During the winter months, advection radiation fog (平流辐射雾) can form quickly in valleys and low-lying areas.

在冬季，advection radiation fog（平流辐射雾）可以迅速在山谷和低洼地区形成。

2.The phenomenon of advection radiation fog (平流辐射雾) often occurs in late autumn when warm air meets cold ground temperatures.

当温暖的空气与寒冷的地面温度相遇时，advection radiation fog（平流辐射雾）现象通常发生在深秋。

3.The coastal area experienced a sudden drop in visibility due to the formation of advection radiation fog (平流辐射雾) as warm, moist air moved over cooler waters.

由于温暖潮湿的空气在较冷的水面上移动，沿海地区的能见度骤然下降，形成了advection radiation fog（平流辐射雾）。

4.Meteorologists warned that advection radiation fog (平流辐射雾) could lead to hazardous driving conditions overnight.

气象学家警告说，advection radiation fog（平流辐射雾）可能会导致夜间驾驶条件危险。

5.Pilots need to be cautious when flying through areas prone to advection radiation fog (平流辐射雾), as it can significantly reduce visibility.

飞行员在飞越容易出现advection radiation fog（平流辐射雾）的地区时需要格外小心，因为这会显著降低能见度。

作文

Fog is a fascinating and complex meteorological phenomenon that can significantly impact weather conditions, visibility, and transportation. Among the various types of fog, advection radiation fog stands out as an intriguing example of how different atmospheric processes interact to create unique weather patterns. Understanding this type of fog requires a grasp of both advection and radiation processes in meteorology. Advection fog occurs when warm, moist air moves over a cooler surface, leading to condensation of water vapor into tiny droplets that form fog. This process is primarily driven by wind, which transports the warm air mass from one location to another. In contrast, radiation fog forms during clear nights when the ground loses heat rapidly through radiation, causing the air near the surface to cool down and condense into fog. When these two processes combine, we observe what is referred to as advection radiation fog (平流辐射雾).This type of fog typically forms at night or during the early morning hours when the temperature drops significantly. For instance, if a warm, moist air mass moves over a cooler body of water or land, the temperature difference can lead to the formation of fog. The moisture in the air condenses as it cools, creating a thick layer of fog that can reduce visibility to dangerous levels. This phenomenon is particularly common in coastal regions where warm ocean currents meet cooler air masses.The implications of advection radiation fog are significant, especially for transportation. Drivers and pilots must be cautious when navigating through foggy conditions, as visibility can drop dramatically. This type of fog can also affect maritime activities, leading to delays in shipping and fishing operations. Therefore, understanding the conditions that lead to the formation of advection radiation fog is crucial for safety and planning.Meteorologists utilize satellite imagery and weather models to predict the occurrence of this fog. By analyzing temperature gradients and moisture levels in the atmosphere, they can provide forecasts that help people prepare for potential foggy conditions. Accurate weather predictions are essential for minimizing the risks associated with advection radiation fog, ensuring that individuals and industries can take appropriate precautions.In conclusion, advection radiation fog is a remarkable intersection of atmospheric phenomena that showcases the dynamic nature of our weather systems. By understanding the mechanisms behind its formation, we can better appreciate the complexities of meteorology and the importance of accurate weather forecasting. As our climate continues to change, studying such phenomena becomes even more critical for ensuring public safety and effective transportation management.