1. High humidity: a temperature dew point "spread of 4 degrees" or less
2. Calm wind: "less than 5 knots" moist air remains concentrated near the ground
3. Temperature droping: night time and/or cold front passage
is also known as ground fog. All fog is exactly the same as a cloud except a cloud forms hundreds or thousands of feet above the ground where as ground fog is touching the ground
think of the air as similar to a sponge, both can hold water, if too much water is added to a sponge the excess pours out, and if a sponge holding even small amounts of water is squeezed it will release some water. Cooling any air mass (large volume) makes it less able to hold water vapor (squeezing the sponge) water vapor collects on grass (dew) or dust (cloud/fog)
1. High humidity resulting in a temperature dew point spread of 4 degrees or less (best example: ground wet from recent rain fall orair near ground absorbes a water (a lot over a few hours)
2. Light or no wind( best example; winds usually are calmer at night, so moist air stays concentrated near ground (50'-300')instead of winds mixing air with dry air from above & around area )
3. A temperature drop of the air near the ground( best example: later in the evening if/when clear skies occur the suns heat in the surface of the ground is released upward as radiated heat into space the ground cools and cools the nearby air. Cool air can not hold as much water vapor as hot air, so the water vapor collects on tiny floating dust/smoke particles just like a cold can of any drink will be wet after a couple minutes out of the refigerator
The water vapor da yall some dummies who ant know dat
At the North Pole, the spring conditions can be cloudy. The fog and clouds is from the water evaporating from the melting snow surface. Radiation energy is trapped near the surface, so the temperatures recently increased to a warm temp of 27 F.
conditions that favor the reverse reaction
microwave background radiation is a thermal radiation left from the early stage of universe when it was much small and much hotter and filled with uniformly distributed opaque fog of hydrogen plasma
Afternoon thunderstorms
i won't say it
Cool, clear, and calm conditions favor the formation of fog by radiation cooling.
Cool, clear, and calm conditions favor the formation of fog by radiation cooling.
The type of fog that forms in valleys at night is Radiation Fog. It usually does not last long after sunrise.
radiation fog
London fog : radiation fog enhanced by pollutants. Wisconsin fog : evaporation fog near water.
H2O nearing dew point by radiative process causes radiation fog . Advection of warm air over cold surface makes Avection fog
insignificantly.
There are two types of fog, advection fog and radiation, or ground fog. Advection fog is common along the pacific coast of the United States. Warm, moist air over the Pacific Ocean is blown inward. The other kind of fog is radiation, or ground fog. This fog is common lots of places. It forms when a layer of warm, moist air forms low to the ground.
Radiation Fog
radiation fog
Penumbra is the excess fog from scatter radiation
fog and natural disaters