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The anvil is not part of the tornado, it is part of the parent thunderstorm. The anvil forms when the storm cloud grows upward until hitting a layer of stable air that it cannot rise through. This causes the top of the storm to flatten and spread out.
The first stage is the cumulus cloud stage in which the fluffy cumulus cloud in an unstable (warm and moist near surface and very cold aloft) builds into a towing cumulus. All we have is an updraft! In the next stage, the mature stage rain begins to fall dragging down cool air and evaporating into the downdraft and cooling it. Then we have an updraft and a downdraft together. When the mature thunderstorm reaches way up in the atmospehere to the tropopause (boundary between the layer of the atmospehere where sensible weather occurs and the stratosphere) an anvil shape becomes evident. The final stage is the dissipating stage. The rain and rain cooled air become so dominant that the updraft dies and all that is left is the downdraft. The thunderstorm dies without an updraft.
Cirrus are high altitude clouds. Cumulo nimbus (anvil shaped clouds) indicate the possibility of rain.
A Thunderstorm cloud is called cumulonimbus cloud. They can range in height from 30,000 feet to 70,000 feet into the atmosphere. The taller the cloud, the more power that has built up within it.
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An anvil cloud is an anvil shaped structure at the top of a thunderstorm that results from the updraft hitting stable air, flattening, and spreading out.
The anvil is not part of a tornado nor is it directly related to tornadoes. When a thunderstorm forms, is produces a tall cloud called a cumulonimbus. The cloud rises until it reaches a stable layer, at which point the top spreads out flat. This flat top to the thunderstorm cloud is called the anvil. Most tornadoes are produced by a kind of thunderstorm called a supercell. Supercells usually have very well shaped anvils.
An anvil cloud is a tall, anvil-shaped thundercloud.
No. The anvil is part of the thunderstorm. Namely it is that part of the cloud that spreads out at the top. Tornadoes form from thunderstorms.
An incus in Latin is an anvil (and, in medical terminology, an anvil-shaped bone of the middle ear).
The anvil is not actually part of a tornado. it is part of the storm that produces a tornado. Inside a thunderstorm moist air rises as long as it is warmer than its surroundings. However, when the rising cloud of the thunderstorm reaches a comparatively warm layers such as at the top of the troposphere it cannot rise any more, and will spread out, forming a wide, flat top to the storm cloud. This flat top is the anvil.
The anvil is not part of the tornado, it is part of the parent thunderstorm. The anvil forms when the storm cloud grows upward until hitting a layer of stable air that it cannot rise through. This causes the top of the storm to flatten and spread out.
The presence of an anvil shape in a thunderstorm is typically a result of powerful updrafts within the storm. As the warm, moist air rises rapidly, it reaches the top of the storm and spreads out horizontally. This spreading out forms the flat, anvil-shaped top of the cloud, which is often associated with severe thunderstorms and can indicate the presence of strong winds and potential for severe weather.
Cloud lighting
The first stage is the cumulus cloud stage in which the fluffy cumulus cloud in an unstable (warm and moist near surface and very cold aloft) builds into a towing cumulus. All we have is an updraft! In the next stage, the mature stage rain begins to fall dragging down cool air and evaporating into the downdraft and cooling it. Then we have an updraft and a downdraft together. When the mature thunderstorm reaches way up in the atmospehere to the tropopause (boundary between the layer of the atmospehere where sensible weather occurs and the stratosphere) an anvil shape becomes evident. The final stage is the dissipating stage. The rain and rain cooled air become so dominant that the updraft dies and all that is left is the downdraft. The thunderstorm dies without an updraft.
Yes. That is the shape most thunderstorms take, whether they are tornadic or not.