The correct spelling is tule fog instead of tulie fog. Tule fog is defined as a thick ground fog in areas of California's Great Central Valley. Tule fog forms in late fall after the first significant rainfall until spring.
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∙ 9y agoTule fog is a dense fog that forms in California's Central Valley during the fall and winter months. It is caused by moist air cooling rapidly at night, creating foggy conditions that can reduce visibility to near zero. Tule fog can be hazardous for drivers on the road.
The four types of fog are radiation fog, advection fog, upslope fog, and evaporation fog. Radiation fog forms on cool, clear nights when the ground loses heat rapidly. Advection fog occurs when warm, moist air moves over a cold surface. Upslope fog is formed when moist air is forced to rise up a slope or mountain. Evaporation fog occurs when air near the surface is cooled to its dew point by evaporation.
Steam fog is fog that that comes off of water. It comes up when it is really ht outside.
The fog that results from the nightly cooling of the earth is called radiation fog. It forms when the ground cools rapidly, causing the air near the surface to cool and reach its dew point, leading to condensation and fog formation.
fog is closer to the ground
"Fog wreaths" typically refers to thick, swirling formations of fog that can resemble wreaths or coils. These fog formations can create a mysterious, atmospheric effect and impact visibility in the surrounding area.
It was Gerard Gordeau vs Teila Tulie at UFC 1, held in Denver Colorado November 12, 1993. Gordeau won by doctor stoppage via kicking Tulie in the face and sending one of his teeth flying to the commentary table.
Freezing fog, advection fog, and evaporation fog!
London fog : radiation fog enhanced by pollutants. Wisconsin fog : evaporation fog near water.
Pea soup fog is fog that is extremely thick, or heavy.
fog = Nebel fog = Schleier (figurative)
The adjective form of "fog" is "foggy."
Fog intensity refers to the density or thickness of fog in a particular area. It is a measure of how much visibility is reduced due to fog, with higher intensity indicating thicker fog and lower visibility. Fog intensity can vary depending on factors such as temperature, humidity, and wind conditions.
in the fog
There is no prefix for fog.
"Fog-laden" describes an area that is covered or filled with fog, often implying that the fog is thick or heavy in that place. It suggests reduced visibility due to an abundance of fog in the atmosphere.
The fog that results from the nightly cooling of the earth is called radiation fog. It forms when the ground cools rapidly, causing the air near the surface to cool and reach its dew point, leading to condensation and fog formation.
Thin fog is a type of fog that has lower visibility compared to other types of fog, such as thick fog. It can occur when moisture in the air condenses into tiny water droplets close to the ground, creating a haze-like appearance. Thin fog tends to disperse more quickly than thicker fog when conditions change.