Radiation fog is a type of ground-level stratus cloud that forms when the air near the surface cools to its dew point due to radiational cooling. This typically occurs on clear nights with little wind, allowing heat from the Earth’s surface to escape into space.
The dissipation of radiation fog is influenced by two main factors: wind speed and solar insolation. Wind can mix the air near the ground with warmer air above, reducing the temperature difference that sustains the fog. Solar insolation provides heat to the surface, which can also lead to the evaporation of water droplets in the fog.
A = insolation factor (W/mΒ²)
B = wind speed (m/s)
C = constant (hours)
What factors affect the dissipation of radiation fog?
How does wind speed impact fog dissipation?
What role does solar insolation play in fog dispersion?
Can you explain what radiation fog is?
How do I use this calculator for fog dissipation time?
What conditions are ideal for the formation of radiation fog?
Why is it important to know the dissipation time of radiation fog?
Results are for informational purposes only and do not constitute professional advice.
