What is an adventure fog?
Adveting fog is a fog that is produced when humid air moves over a surface that is colder than air. Most often you can see on the seas or other water bodies, but it is possible despite the snowy or freezing masses of soil. When the air temperature is reduced to its dew point, it begins to change. First, saturation occurs. Then fog.
In areas where sea air is cooled with water, the most common fog. As a result, this fog is also called sea fog. Counseling fog is usually seen during certain seasons, specifically in the spring and in the first few months of the summer. At that time, the surface temperature of the seawater is either at the lowest temperature or is recovering from the winter season, where it was already the lowest. Britain is surrounded by sea and sea air almost always approaches the Earth from the southwest. As a result, the advice is in this with quite common grounds of the country. There are regional names throughout Britain for the same occurrence. For example, "Fret" is common next to the Northumbrian coast and "haar" is inIdet in the southeastern part of Scotland.
Some areas seem to be more joyful fog than others. For example, in Newfoundland, this is typical of four days of every ten, especially in July. This is because there is a great current called the Labrador current in the sea that creates a fog when the warmer air hits it.
Other areas where the fog of advice is common, includes Oya Shio and Kamchatka in the Pacific Ocean. In addition, there are areas of higher latitudes, where it is above ice with packaging and in the waters of open ocean, even in the summer months. These areas include Antarctica, Canadian archipelago and parts of the Arctic Ocean.
Costal Advention fog is seen when the Extremely Cold Water moves parallel to subtropical continents. Canary currents near Northwest Africa, a stream of Benguel near Southwest Africa and Humbolt Current near Chile are one of the nThe more famous cold water streams that work on low -level air cooling. As a result, these areas often have councilor's fog.
If the wind is less than 30 nodes in the above areas, the fog remains in place. Alternatively, if the wind is stronger, the fog lifts. As a result, they form stratiform clouds.