What makes mist moist

Britannica English: Translation of moist for Arabic Speakers. Subscribe to America's largest dictionary and get thousands more definitions and advanced search—ad free! Log in Sign Up. Save Word. Definition of moist. Other Words from moist moistly adverb. Synonyms for moist Synonyms damp , dampish , dank , wettish Visit the Thesaurus for More. Choose the Right Synonym for moist wet , damp , dank , moist , humid mean covered or more or less soaked with liquid.

Examples of moist in a Sentence I love cookies when they are moist and chewy. The pork chops were tender and moist. She dabbed her moist eyes with a handkerchief.

Fog is formed when warm moist air moves over a cold surface. The eggs will hatch sooner in warm, moist conditions. First Known Use of moist 14th century, in the meaning defined at sense 1. Buying Guide Our team at The Usage has selected the best dehumidifiers of Learn More About moist. Time Traveler for moist The first known use of moist was in the 14th century See more words from the same century. Style: MLA. More Definitions for moist.

English Language Learners Definition of moist. Kids Definition of moist. Other Words from moist moistness noun. Mist can reduce visibility to between one and two kilometers. Types of Fog There are several different types of fog, including radiation fog, advection fog, valley fog, and freezing fog. As heat is transferred from the ground to the air, water droplets form. Ground fog does not reach as high as any of the clouds overhead.

It usually forms at night. Advection fog forms when warm, moist air passes over a cool surface. This process is called advection , a scientific name describing the movement of fluid.

In the atmosphere, the fluid is wind. When the moist , warm air makes contact with the cooler surface air, water vapor condenses to create fog. Advection fog shows up mostly in places where warm, tropical air meets cooler ocean water. The Pacific coast of the United States, from Washington to California, is often covered in advection fog.

The cold California Current , which runs along the western coast of North America, is much cooler than the warm air along the coast. Valley fog forms in mountain valleys, usually during winter.

Valley fog develops when mountains prevent the dense air from escaping. The fog is trapped in the bowl of the valley. In , vapor condensed around particles of air pollution in the Meuse Valley, Belgium.

More than 60 people died as a result of this deadly valley fog. Freezing fog happens when the liquid fog droplets freeze to solid surfaces. Mountaintops that are covered by clouds are often covered in freezing fog. As the freezing fog lifts, the ground, the trees, and even objects like spider webs, are blanketed by a layer of frost.

The white landscapes of freezing fog are common in places with cold, moist climates, such as Scandinavia or Antarctica. Fog Catchers Many ancient cultures collected water from fog by placing large pots under trees and shrubs.

As the water from fog collected on these objects, the pots collected the water. This method of water collection was effective, but not as effective as collecting rainwater or other liquid water. Today, engineer s are working on more sophisticated ways to collect water from fog. As fog glides in, water droplets form around the thin screens and drip to the collection pools below.

In one day, a single screen can collect more than a hundred gallons of water. The village of Bellavista, Peru, relies on fog catchers. Bellavista is an area that has little access to liquid water—no rivers, lakes, or glaciers are nearby. Wells dry up quickly. Water for irrigation and human consumption is threatened. Every year, however, huge fogs blow in from the Pacific Ocean. In , the community invested in a series of fog catchers outside of town.

Now, the residents of Bellavista have enough water to irrigate trees and gardens, as well as provide for their own drinking and hygiene needs. Engineers warn that fog catchers will only work in small areas. Still, engineers and politicians are working on ways to make more powerful fog catchers that will perhaps reduce the need for people to rely so much on groundwater.

Pea Souper A "pea souper" is a type of fog that forms when water condenses around microscopic particles of coal. This fog is often a brownish-yellow color, leading to the name. Pea soupers are common in areas that burn coal for energy. The London Fog of , which killed 12, people around the urban center of London, England, was a pea souper. The Great Fog led to legislation that regulated the coal industry and air pollution in the United Kingdom.

The cold Labrador Current from the north and the warm Gulf Stream current from the east create prime conditions for thick fog to form almost every day. Gas molecules are in constant, random motion. Also called radiation fog. Also called the Arctic Current. There has been a bridge on the site for more than 2, years. Also called ground fog. The audio, illustrations, photos, and videos are credited beneath the media asset, except for promotional images, which generally link to another page that contains the media credit.

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