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  2. www.metoffice.gov.uk › fog › coastal-fogCoastal fog - Met Office

    Coastal fog is usually a result of advection fog which forms when relatively warm, moist air passes over a cool surface. In the UK, the most common occurrence of coastal fog is when warm air...

    • Radiation Fog
    • Valley Fog
    • Advection Fog
    • Upslope Fog
    • Evaporation Fog

    Radiation fog usually occurs in the winter, aided by clear skies and calm conditions. The cooling of land overnight by thermal radiation cools the air close to the surface. This reduces the ability of the air to hold moisture, allowing condensation and fog to occur. Radiation fog usually dissipates soon after sunrise as the ground warms. An excepti...

    Valley fog forms where cold dense air settles into the lower parts of a valley, condensing and forming fog. It is often the result of a temperature inversion, with warmer air passing above the valley. Valley fog is confined by local topography and can last for several days in calm conditions during the winter.

    Advection fog occurs when moist, warm air passes over a colder surface and is cooled. A common example of this is when a warm front passes over an area with snow cover. It is also common at sea when moist tropical air moves over cooler waters. If the wind blows in the right direction, then sea fog can become transported over coastal land areas.

    Upslope fog or hill fog forms when winds blow air up a slope (called orographic uplift). The air cools as it rises, allowing moisture in it to condense.

    Evaporation fog is caused by cold air passing over warmer water or moist land. It often causes freezing fog, or sometimes frost. When some of the relatively warm water evaporates into low air layers, it warms the air, causing it to rise and mix with the cooler air that has passed over the surface. The warm, moist air cools as it mixes with the cold...

  3. Fog that forms over water is commonly referred to as sea fog or lake fog. It forms when warm, moist air flows over relatively colder waters. Sea or lake fog can occur over the Atlantic and Pacific Oceans, the Gulf of Mexico, the Great Lakes and other bodies of water.

  4. Jun 10, 2019 · Coastal fog forms when moist, warm air passes over a cooler surface. When warm air blows across the surface of a body of water, it passes over cool air just above the surface of the water, and becomes condensed, forming small water particles that create fog.

    • Geoffrey Migiro
  5. Sea fog, a type of advection fog, can occur when warm, wet, air rolls off the land and onto the colder sea, or when a warm weather front hits a cold ocean current. In the UK, the north-east coast is very prone to sea fog because of the cold waters of the North Sea.

  6. Sea fog occurs when the wind pushes warm, moist air over a cooler sea surface. The sea surface cools the air directly above it, causing water vapour to condense into fog. Around New Zealand, high pressure to the east of the country is a good situation for sea fog to form – with northeasterly winds bringing air down from the sub-tropics ...

  7. education.nationalgeographic.org › resource › fogfog

    Oct 19, 2023 · Sea fog, which shows up near bodies of salty water, is formed as water vapor condenses around bits of salt. Depending on the humidity and temperature, fog can form very suddenly and then disappear just as quickly.

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