Fog is created when tiny water droplets or ice crystals become suspended in the air near the Earth's surface. This makes the air less transparent, resulting in reduced visibility.
The Science Behind Fog Formation
Several factors contribute to fog formation:
-
Cooling: When warm, moist air cools, it can no longer hold as much water vapor. The excess water vapor then condenses around microscopic particles in the air (like dust or pollutants), forming tiny water droplets that constitute fog. This is often seen in the evening as the ground cools. The National Weather Service explains that horizontal movement of warm, moist air over a cold surface can also cause this cooling and subsequent condensation.
-
Evaporation: Fog can also form when water evaporates into the air, saturating it to 100% humidity. This can happen when rain falls through cold, dry air, causing the dew point to rise and resulting in saturation. This process is detailed in the Fog Definitions resource.
-
Pollution: Areas with higher levels of pollution often experience thicker fogs. The increased number of particles in the air provides more surfaces for water droplets to condense around, leading to larger droplets and denser fog. This is highlighted in the provided text stating that the thickest fogs tend to occur in industrial areas due to more pollution particles.
Types of Fog (Brief Overview)
While not explicitly asked, understanding the different types of fog helps clarify the formation process. Various types of fog exist, each formed under slightly different atmospheric conditions. These differences primarily involve the mechanisms leading to the cooling or saturation of the air. For a more detailed understanding, refer to resources like Study.com's lesson on fog.
Predicting Fog
Accurately predicting fog is complex, dependent on many factors including temperature, humidity, wind speed, and air pressure. Resources like RainViewer's blog discuss the challenges of fog forecasting. However, understanding the basic mechanisms above provides a foundation for making educated predictions based on local conditions.