radiational cooling - In meteorology, the result of radiative cooling of the earth's surface and adjacent air.
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The cooling of the Earth's surface. At night, the Earth suffers a net heat loss to space due to terrestrial cooling. This is more pronounced when you have a clear sky.
Radiational Cooling - The cooling of the lower atmosphere during the nighttime hours. This, in combination with light surface winds and relatively clear skies, will often set the stage for fog.
The process by which the earth's surface and adjacent air cool by emitting infrared radiation.
RADIATIONAL COOLING- The earth's surface cooling by emitting longwave radiation. The best radiational cooling occurs on clear nights.
produces condensation in the air layers immediately above the ground. If only a thin layer of moist air is present, Dew will form; if a thicker layer is present, radiation fog (and dew) will form.
Radiational CoolingThe cooling of the Earth's surface. At night, the Earth suffers a net heat loss to space due to terrestrial cooling. This is more pronounced when you have a clear sky.
Fog created when at the earth's surface lowers the temperature of the air near the ground to or below its initial dew point. Primarily takes place at night or early morning.
Related term: radiation fog
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RADIATIONAL COOLING The cooling of the earth's surface and the adjacent air. Although it occurs primarily at night, it is whenever the earth's surface suffers a net loss of heat due to the reradiation of surface heat. See terrestrial radiation.
Nocturnal InversionUsed interchangably with Radiational Inversion; a temperature inversion that develops during the night as a result of of the surface.
Like friction, the effects of insolation and radiational cooling are strongest within this layer.
It is within this layer that temperatures are most strongly affected by daytime insolation and nighttime , and winds are affected by friction with the earth's surface.
Used interchangably with Radiational Inversion; a temperature inversion that develops during the night as a result of radiational cooling of the surface.
MOUNTAIN BREEZE A katabatic wind, it is formed at night by the along mountainsides. As the slopes become colder than the surrounding atmosphere, the lower levels of air cool and drain to the lowest point of the terrain.
Since warm air is less dense than cool air, the air over land contracts in response to radiational cooling from the ground below.
Radiation fog - A ground-level fog formed by nocturnal of a humid air layer so that its relative humidity approaches 100 %; sometimes called ground fog.
Radio waves - Long-wavelength, low-frequency electromagnetic waves.
A local wind which develops due to cool, dense air flowing downhill. The cooler air is generally a result of night time radiational cooling in the lower layers of the atmosphere, but katabatic winds also occur over snow fields and glaciers.
Radiation fog Fog produced over land when reduces the air temperature to or below its dew point. It is also known as ground fog and valley fog.
radiation fog—Fog characteristically resulting when radiational cooling of the earth's surface lowers the air temperature near the ground to or below its initial dew point on calm, clear nights.
There are four common causes of a temperature inversion: , advection of warm air over cold air as in frontal situations, advection of warm air over a cold surface such as snow or ice, and subsidence, ...
See also: Air, Surface, Weather, Temperature, Radiation