what is the difference between cloudy and mostly cloudy?
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“Partly cloudy” refers to cloud coverage from two through five tenths; “mostly cloudy” is used in reference to six through nine tenths cloud coverage; and “cloudy” to a complete or nearly complete overcast.
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Showers, also known as rain showers, have a shorter duration than rain. ... Compared to rain, showers cover a smaller area but can be more intense. Cumulonimbus clouds (thunderstorm clouds) produce the heaviest rainfalls. Showers from stratocumulus clouds (not as puffy) tend to not be so heavy.
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Cloudy vision can also be a result of changes in or damage to the cornea, (the clear bit at the front of your eye) including infections or inflammations. Less common conditions that may contribute to cloudy vision include: diabetes, optic nerve disease and macular degeneration.
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As adjectives the difference between gloomy and overcast is that gloomy is imperfectly illuminated; dismal through obscurity or darkness; dusky; dim; clouded while overcast is covered with clouds; overshadowed; darkened.
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That is because clouds are classified and named according to their altitudes, the ways they form, and their general characteristics. The three main types of clouds are cirrus, cumulus, and stratus. These names come from Latin words that suggest the clouds' appearances. appear feathery or wispy.
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Low-pressure systems are associated with clouds and precipitation that minimize temperature changes throughout the day, whereas high-pressure systems normally associate with dry weather and mostly clear skies with larger diurnal temperature changes due to greater radiation at night and greater sunshine during the day.
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A cloud is made of water drops or ice crystals floating in the sky. There are many kinds of clouds. Clouds are an important part of Earth's weather.
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As nouns the difference between humidity and fog is that humidity is dampness, especially that of the air while fog is (label) a thick cloud that forms near the ground; the obscurity of such a cloud or fog can be a new growth of grass appearing on a field that has been mowed or grazed.
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Whereas showers are much more scattered and shorter in duration than rain, and that not everyone in the locality will get wet at the same time, or even get wet at all. ... Convective rain falls from cumuliform clouds, such as cumulus and cumulonimbus. We call these showers, and they tend to be short-lived.
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All in all, there are ten fundamental types of clouds. Often, you'll some places simply class clouds as cirrus, stratus, and cumulus because these clouds are the most common and representative for each altitude class. High-level clouds (5-13 km): cirrocumulus, cirrus, and cirrostratus.
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Cumulus clouds look like fluffy, white cotton balls in the sky. They are beautiful in sunsets, and their varying sizes and shapes can make them fun to observe! Stratus cloud often look like thin, white sheets covering the whole sky. Since they are so thin, they seldom produce much rain or snow.
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Thicker clouds look darker than thinner ones, which let more light through and so appear white. Richard Brill, a professor at Honolulu Community College, gives this answer: It is the thickness, or height of clouds, that makes them look gray. Clouds are made of tiny droplets of water or ice.
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Mostly cloudy means that from 80 to 90 percent of the sky will be covered by clouds.” Q: What does overcast mean? A: Overcast means almost all of the sky is cloud covered, he adds. “An overcast sky is usually a dull and gray-looking sky when clouds are expected to cover all of the surrounding area.
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What is the difference between cirrus and cumulus clouds? Cirrus clouds are thin; cumulus clouds are globular. What condition is required for cloud formation in the atmosphere? A rising parcel of air reaches its dew-point temperature.
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Fog is a cloud that reaches ground level, even if that "ground" is a hill or mountaintop. Mist forms wherever water droplets are suspended in the air by temperature inversion, volcanic activity, or changes in humidity. Fog is denser than mist and tends to last longer.
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Clouds (water vapor) are part of the whole always-moving atmosphere of the earth. We just notice the movement of the clouds because we can see them. The rest of the air is moving too. ... All this movement comes about because different parts of the earth's atmosphere are heated to different levels by the sun.
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Clouds are formed when moist air rises upward. As the air rises, it becomes colder. Eventually the air can't hold all of the water vapor in it, and some of the water vapor condenses to form tiny water droplets. When moist air is cooled at the ground, fog is formed in the same way.