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How high from the ground are stratus clouds in meters?
They are bellow 6000 ft
What type of clouds are wispyfeathery-looking clouds that form above 6000 meters?
The wispy, feathery-looking clouds that form above 6,000 meters are called cirrus clouds. These high-altitude clouds are composed of ice crystals and often indicate fair weather, although they can also signal that a change in the weather may be approaching. Cirrus clouds typically appear thin and wispy, resembling strands of hair or feathers.
Which type of clouds are wispy feathery-looking clouds that firm above 6000 meters?
The wispy, feathery-looking clouds that form above 6,000 meters are known as cirrus clouds. These high-altitude clouds are composed primarily of ice crystals and typically indicate fair weather, although they can also signal an approaching storm when they thicken. Cirrus clouds often appear thin and delicate, resembling strands of hair or wisps of cotton.
Are Cirro stratus clouds high clouds?
Yes, cirrostratus clouds are high clouds that form above 20,000 feet in the atmosphere. They are thin, wispy clouds that often cover the sky in a thin veil, causing a halo effect around the sun or moon.
What are clouds that are very high in the atmosphere?
Clouds that are very high in the atmosphere are called cirrus clouds. These clouds are composed of ice crystals and usually appear wispy and thin. They form at altitudes above 20,000 feet and are often associated with fair weather.
Are cirrus or stratus clouds form above 6000 meters?
Cirrus clouds form above 6000 meters, while stratus clouds typically form at lower altitudes. Cirrus clouds are thin and wispy, often seen at high altitudes, while stratus clouds are usually lower in the sky and appear more spread out in a layered formation.
What are the names of the clouds?
The different names for clouds are cirrus, stratus, cumulus, and altostratus. While stratus clouds are at an altitude that is below 6000 feet, cirrus clouds are high clouds that form above 20,000 feet.
How high from the ground are stratus clouds in meters?
They are bellow 6000 ft
What types of clouds are not likely to form below 2000 meters?
Cirrus clouds are not likely to form below 2000 meters as they are high-altitude clouds found above 6000 meters. These clouds are wispy and thin, made up of ice crystals, and are often associated with fair weather.
What type of clouds are wispyfeathery-looking clouds that form above 6000 meters?
The wispy, feathery-looking clouds that form above 6,000 meters are called cirrus clouds. These high-altitude clouds are composed of ice crystals and often indicate fair weather, although they can also signal that a change in the weather may be approaching. Cirrus clouds typically appear thin and wispy, resembling strands of hair or feathers.
Which type of clouds are wispy feathery-looking clouds that firm above 6000 meters?
The wispy, feathery-looking clouds that form above 6,000 meters are known as cirrus clouds. These high-altitude clouds are composed primarily of ice crystals and typically indicate fair weather, although they can also signal an approaching storm when they thicken. Cirrus clouds often appear thin and delicate, resembling strands of hair or wisps of cotton.
What are clouds mostly of ice crystals that form high above earth?
clouds
Is there more air pressure high above the clouds or the clouds or on the ground?
in the air
Is mount Everest high enough to touch the clouds?
To climb high on Mount Everest you have to climb up through the clouds.
Are Cirro stratus clouds high clouds?
Yes, cirrostratus clouds are high clouds that form above 20,000 feet in the atmosphere. They are thin, wispy clouds that often cover the sky in a thin veil, causing a halo effect around the sun or moon.
When air high above the earth surface is cooled below the dew point its is likely to form?
Clouds.
What word describes high thin wispy clouds?
The most usual form of high-level clouds are thin and often wispy CIRRUS clouds. Cirrus clouds are usually found at heights greater than 20,000 feet. Cirrus clouds are composed of ice crystals that originate from the freezing of supercooled water droplets.
