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Fog - Wikipedia Fog is a visible aerosol consisting of tiny water droplets or ice crystals held in the air near the Earth 's surface [1][2] Fog can be considered a type of low-lying cloud usually resembling stratus and is heavily influenced by nearby bodies of water, topography, and wind conditions
Fog | Definition, Formation, Types, Facts | Britannica Fog is a cloud of small water droplets near ground level It is formed by the condensation of water vapor on tiny particles that are always present in natural air; this occurs when the air becomes saturated with moisture
How Fog Forms - National Weather Service Steam fog forms when cold air moves over warm water When the cool air mixes with the warm moist air over the water, the moist air cools until its humidity reaches 100% and fog forms
Dense Tule Fog Descends On California And Stays 3 Weeks California's Central Valley is no stranger to the phenomenon known as tule fog, but a blend of perfect conditions has allowed this particular event to last for over three weeks
The strange science of how fog forms - BBC Science Focus Magazine Fog is made up of molecules of water vapour, suspended in the air as tiny droplets of water but lingering close to the surface Essentially, fog is just cloud that touches Earth’s surface and it forms the same way that clouds do
FOG Definition Meaning - Merriam-Webster The meaning of FOG is vapor condensed to fine particles of water suspended in the lower atmosphere that differs from cloud only in being near the ground How to use fog in a sentence
A. Fog Types - National Weather Service Fog forms when the temperature and dew point of the air approach the same value (i e , dew-point spread is less than 5°F) either through cooling of the air (producing advection, radiation, or upslope fog) or by adding enough moisture to raise the dew point (producing steam or frontal fog)
How Does Fog Form? | Over Land, Over Water, Radiation, Advection . . . Fog is a cloud of small water droplets near ground level It is formed by the condensation of water vapor on tiny particles that are always present in natural air; this occurs when the air becomes saturated with moisture