Sleet is type of precipitation unique from scurrently, hail, and freezing rain. It creates under particular weather conditions, once a temperature invariation reasons scurrently to melt, then refreeze.

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Sometimes the weather forecast advises of “sleet,” fairly than scurrently. When meteorologists in the USA use this term, they are referring to tiny ice pellets (the size of a pea, at most) formed as soon as falling snow melts then quickly refreezes. (In the United Kingdom, sleet typically describes a wintry mix). These pelallows commonly bounce as they hit the ground. Sleet have the right to be dangerous, quickly coating the surchallenge of roadways and making driving hazardous.Sleet Forms in Layers of Air (Warm over Cold)To understand also exactly how sleet forms, it helps to understand how scurrently forms.The air closest to Earth’s surface—the layer wbelow weather happens—is dubbed the tropospbelow. In basic, the higher you go in the tropospbelow, the colder the air becomes.Throughout precipitation formation, if temperatures are at or listed below freezing, 0°C (32°F), at cloud level, water in the air freezes into ice crystals, and the crystals stick together to make snow. The scurrently starts to autumn, and if the air column is freezing cold all the method down from the clouds to the ground, the precipitation stays frozen. It ssuggest falls as scurrently.Sometimes, but, a temperature invariation occurs. Generally, the temperature decreases with boosting altitude. A temperature inversion is when a layer of warm air intrudes in between the ground and the clouds.Under these problems, once the falling snow reaches the layer of warm air, it melts. Then it hits the layer of cold air simply above Earth’s surface and refreezes. This all happens incredibly rapid, and the result is tiny ice pelallows referred to as sleet.Sleet, Freezing Rain, Hail ... What Is the Difference?The problems that lead to freezing rain are comparable to those for sleet: Scurrently falls via a layer of heat air and also melts right into raindrops, then is intercepted by a layer of freezing cold air just above Earth’s surconfront. When that bottom-many layer of cold air is thin, the melted snow does not have actually time refreeze as it falls with. It hits the ground as liquid water—rain—then freezes as it touches a freezing cold surconfront, such as a tree branch, a road, or a bridge.Hail additionally is composed of ice pelallows, yet hailstones are bigger than the tiny pelallows that consist of sleet. Hailstones create as soon as the updrafts produced by thunderstorms (which are even more common in spring and summer than winter) easily lift water droplets high in the troposphere, where they freeze at incredibly low temperatures, then loss.


Term Part of Speech Definition



storm via high winds, intense cold, heavy snow, and bit rain.



form of glass in which a product (traditionally, lead oxide) is included to boost the glass" appearance. Also referred to as lead crystal or crystal glass.



to predict, specifically the weather.

freezing rain


liquid precipitation that hardens to ice as soon as it touches a surface.



precipitation that drops as ice.



act or circumstance of being upside-dvery own.



tiny, rounded object.



all forms in which water drops to Planet from the setting.



rain that freezes as it falls to Earth. Also referred to as ice pellets.



level of hotness or coldness measured by a thermometer through a numerical scale.



lowest layer of the Earth"s atmosphere, extending from the surchallenge to around 16 kilometers (10 miles) over.



state of the atmosphere, including temperature, atmospheric pressure, wind, humidity, precipitation, and cloudiness.

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time of year once part of the Planet receives the least daylight: December, January, and also February in the Northern Hemispbelow and also June, July, and also August in the Southern Hemisphere.