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Fog is a low-lying, visible aerosol cloud that is greatly influenced by nearby bodies of water, topography, and wind conditions. There are many kinds of fog, including radiation, ground, and advection fog. Read on to learn about the different types of fog. Also, learn what causes fog.
Ground fog, also known as smog, is caused by water droplets that are suspended in the air. It generally dissipates when the sun rises. The warming of the air makes it more able to hold vapor and evaporate the water droplets. If the skies are overcast, the ground will not be heated, so ground fog will persist during the day.
Another type of ground fog is advection fog. It forms when warm moist air flows over a cool surface. This type of fog is most prevalent off the coasts of the western United States and the Pacific Ocean. In addition, the California Current, which runs along the west coast of North America, tends to produce advection fog.
Advection fog is a type of weather phenomenon that develops when moist air passes horizontally over a cold surface. Fog can be dense and affect visibility. It is also a common phenomenon during the fall. Generally, the onset of advection fog occurs around sunset or during the afternoon.
Advection fog occurs in many regions around the world. It is particularly common in coastal regions such as the United Kingdom, where sea air approaches the country from the southwest. It has regional names, such as fret in the North and haar in southern Scotland. This weather phenomenon is also common in Newfoundland, where it can occur four days out of every month.
Radiation fog is a type of low-lying fog that occurs in regions with rapid cooling. It forms in low-lying spots in the atmosphere and can affect visibility at airports and other locations. Its onset can be detected from space and is often accompanied by delays and cancellations at airports.
Radiation fog is most commonly seen during the fall and winter months. The air near the ground cools overnight, increasing its saturation level and creating the conditions for fog formation. The fog then forms near the ground, then extends upwards and disappears by morning when the Sun warms the ground.
Drizzle in fog is precipitation with droplets that are smaller than 0.5 millimeters in diameter. It typically occurs during cold spells in deep mountain valleys. This precipitation may be referred to as pogonip, derived from the Shoshone language and meaning "cloud". The Old Farmer's Almanac routinely includes "Beware the Pogonip" in the December calendar. The writer Jack London even describes pogonip in his novel Smoke Bellew.
While fog is the most common type of fog, there are many types of drizzle that are caused by different weather conditions. Drizzle is a type of precipitation that occurs when tiny raindrops collide with other clouds. As these cloud droplets collide, they grow in size.
Drizzle causes multi-vehicle pile-ups
A multi-vehicle pile-up on a busy California highway closed the southbound lanes of Highway 5 near Box Canyon late Friday night. The accident involved a semi and several cars, and caused heavy traffic backups in the area. One person was seriously injured and airlifted to the hospital, while others suffered minor injuries. An out-of-control semi reportedly caused the accident. The California Highway Patrol has issued a travel advisory for the area, warning motorists to expect delays and encouraged them to use alternative routes.
In one deadly accident in the Dallas-Fort Worth area, a 134-car pile-up closed Interstate 35 West. It's not clear what caused the crash, but it appears that the icy conditions triggered a chain reaction. According to police, the road was slick and icy due to freezing rain. The Fort Worth Fire Department called it a mass casualty accident.
Drizzle causes freezing drizzle
Driving conditions across northeastern Colorado are slick because of freezing drizzle. This weather condition is expected to continue all afternoon and may briefly change to snow before ending later tonight. The icy roads are particularly hazardous on the north and west sides of the Denver area. Other places where icy roads and sidewalks are reported include Boulder and Loveland.
The key to determining the exact definition of freezing drizzle is to first understand what causes it. This kind of precipitation is caused by supercooled water that remains in liquid form at freezing temperatures. It is formed when there is a low-level cloud deck that is almost entirely made of liquid water. The freezing drizzle is characterized by the accumulation of small liquid particles and the consequent super cooling of these particles as they head toward the ground.
Mist or haze
In a cloudy day, the visibility of an object may be reduced. This phenomenon can be caused by a combination of two main factors: moisture content and temperature. In humid climates, mist is the result of small water droplets suspended in the air, while in dry climates, it's the result of large numbers of dry particles suspended in the air.
In some climates, mist or haze can be caused by air pollution. This kind of air pollution is often caused by temperature differences. It can appear as a soft haze or light fog.
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