Sea fog, also known as marine stratus, is a type of fog that forms over coastal areas when the air temperature near the surface is cooled to its dew point. This cooling typically occurs due to the transfer of heat from the warm air to the cold water surface.
The probability of sea fog formation can be influenced by several factors, including Sea Surface Temperature (SST) and air temperature. Generally, a smaller difference between SST and air temperature increases the likelihood of fog formation.
T_{text{air}} = Air temperature (Β°C)
T_{text{SST}} = Sea Surface Temperature (Β°C)
T_{text{threshold}} = Threshold temperature difference for fog formation (Β°C)
What is sea fog?
How does Sea Surface Temperature (SST) affect sea fog formation?
What factors influence the probability of sea fog?
Can you explain how sea fog forms over coastal areas?
Why is there a difference between SST and air temperature in sea fog formation?
How does this calculator help with understanding sea fog?
What is the significance of sea fog in coastal areas?
Results are for informational purposes only and do not constitute professional advice.
