No, the highest cloud is the noctilucent cloud, which forms in the mesosphere. Cirrus clouds are high altitude clouds, but not the highest.
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Noctilucent clouds can be seen on clear midsummer evenings that form on the border between earth and space. So they are the highest.
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Noctilucent clouds are the highest clouds in the Earth's atmosphere. They are located in the mesosphere at altitudes of around 76 to 85 kilometres (47 to 53 mi). They are normally too faint to be seen, and are visible only when illuminated by sunlight from below the horizon while the lower layers of the atmosphere are in the Earth's shadow.
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One of the rarest types of clouds is the noctilucent cloud, which is a type of cloud that forms in the mesosphere at very high altitudes. They are typically seen in polar regions during the summer months and can appear to glow in the twilight sky.
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Noctilucent clouds have been documented at heights of 76 to 85 kilometers (47-53 miles). http://science.nasa.gov/headlines/y2008/25aug_nlc.htm
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A low level cloud is a cloud that forms below 6,500 feet (2,000 meters) in the atmosphere. These clouds are typically composed of water droplets and are often associated with precipitation. Examples of low level clouds include stratus clouds, cumulus clouds, and stratocumulus clouds.
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Miscellaneous clouds are types of clouds that don't belong to any specific cloud formation category. They include various cloud formations that don't fit neatly into the standard classifications, sometimes due to their unique appearance or formation process. Examples include the mammatus, noctilucent, and fallstreak hole clouds.
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The highest cloud type is called noctilucent clouds, which form in the mesosphere, about 50 miles above the Earth's surface. They are only visible during twilight and are made up of tiny ice crystals.
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With the exception of rare stratospheric noctilucent clouds, cirrus forms the highest cloud layer (also cirrostratus or cirrocumulus). In the tropics (where the troposphere is thicker, that is tropopause is higher) cirrus can generally occur up to 50-60,000 feet (15-18000 metres), sometimes higher when associated with tropical cumulonimbus anvils.
Note that the possible height of cloud varies with location and airmass, so the highest cloud can occur in the tropics, the lower heights (with cirrus possible at 10,000 ft or 3500 m) in polar regions.
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Noctilucent clouds are found in the mesosphere, which is the third layer of Earth's atmosphere. They form at altitudes of around 50 miles (80 kilometers) above the Earth's surface and are visible only during astronomical twilight.
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You may be referring to noctilucent clouds.
http://www.spaceweather.com/nlcs/gallery2008_page1.htm
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High-level clouds include cirrus, cirrostratus, and cirrocumulus. Middle-level clouds include altocumulus and altostratus. Low-level clouds include stratocumulus, stratus, and nimbostratus.
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Noctilucent clouds are composed of ice crystals that form in the upper atmosphere, specifically in the mesosphere at altitudes of 50 to 85 km (31 to 53 miles). The ice crystals are composed of water and other compounds, like meteoric dust and chemicals released by volcanic eruptions. These materials combine to create the thin, wispy clouds that glow at night when illuminated by the Sun below the horizon.
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Yes. Noctilucent clouds are a rare type of thin cloud that form in the mesosphere in the higher latitudes. These clouds are so thin that they can only been seen when lit from below in the evening or at dawn.
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Noctilucent clouds are the highest and are made of crystals of water ice. They are located in the Mesosphere some 76 kilometers high
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It's called in-cloud or cloud-to-cloud lightning.
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It's called in-cloud or cloud-to-cloud lightning.
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Yes, "cloud" can function as a preposition when used in phrases like "in the cloud" or "above the cloud." In these cases, it shows the relationship between an object and its location in relation to the cloud.
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Cloud-to-cloud lightning is commonly referred to as intracloud lightning because it occurs entirely within the same cloud without reaching the ground.
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cirrocumulus clouds range above 18,000 feet but cumulonimbus clouds range from near ground to above 50,000 feet.
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There are three main types of lightning strikes: cloud-to-ground strikes, intra-cloud strikes, and cloud-to-cloud strikes. Cloud-to-ground strikes are the most common and well-known type, where lightning extends from the cloud to the ground. Intra-cloud strikes occur within the cloud itself, and cloud-to-cloud strikes happen between different clouds.
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Depending on context, cloud can be translated as:
Noun
Wolke (cloud in the sky)
in Misskredit (as in: to be under a cloud)
Schutz (as in: under the cloud of night)
Verb
sich bewölken
trüben
vernebeln
verdüstern
verschleiern
verdunkeln
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There are 3 main places lightening can travel from. The ground to a cloud, a cloud to a cloud, and the cloud to the ground.
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Cloud base refers to the altitude above the ground at which the lowest portion of a cloud is observed. Cloud ceiling, on the other hand, is the height above the ground of the lowest cloud layer covering more than half of the sky. Cloud base is the specific altitude at which a cloud starts, while cloud ceiling is the overall height of the lowest cloud layer in the sky.
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An accessory cloud is a type of cloud that forms in conjunction with a larger, main cloud system. These clouds typically surround or are located adjacent to the main cloud, and they may indicate changes in atmospheric conditions or provide additional information about the main cloud system.
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A cumulus cloud is a fluffy, white cloud that usually indicates fair weather, while a cumulonimbus cloud is a larger, towering cloud that can bring thunderstorms and severe weather.
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No, the dark base of a tornado is called the funnel cloud. The wall cloud is a lowered cloud base associated with rotating updrafts that sometimes precede tornado formation.
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There is at least one video of such an event occurring.
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Cloud cover is a noun. "Expect lots of cloud cover today."
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The low-altitude billowy cloud is called cumulus cloud.
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It's called in-cloud or cloud-to-cloud lightning.
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The nimbostratus cloud is a somewhat shapeless, widespread, low-sitting cloud which broadly distributes precipitation. The nimbostratus cloud is usually an indication of steady, consistent rainfall.
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A regular rain or snow cloud is commonly known as a cumulonimbus cloud for rain and a nimbostratus cloud for snow.
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