When frozen rain moves up and down within an anvil cloud, it can lead to the formation of hail. The repeated cycling of ice particles through the cloud allows them to accumulate layers of supercooled water, which freeze upon contact. Once they become too heavy to be supported by the updrafts, they fall to the ground as hailstones. This process is typical in severe thunderstorms with strong updrafts.
It is usually just called a debris cloud or dust whirl.
Hail forms in cumulonimbus clouds, which are large, dense, and towering clouds associated with thunderstorms. Within these clouds, strong updrafts carry raindrops high into the atmosphere where they freeze, forming hailstones. These hailstones can grow larger as they are then circulated within the storm cloud before eventually falling to the ground.
This type of cloud would be known as a stratus cloud
The cloud formation before a tornado funnel forms is typically a rotating wall cloud. This type of cloud is often associated with severe thunderstorms and can indicate that a tornado may develop. It is important to take shelter if you see a rotating wall cloud, as it could produce a tornado.
a cloud that forms a layer with other flat,clouds is a
An anvil cloud, also known as a cumulonimbus incus, is a large, flat cloud that often forms at the top of a mature thunderstorm. It is typically formed when the updraft of warm air reaches the tropopause and spreads out horizontally. Anvil clouds can indicate severe weather such as heavy rain, thunder, lightning, and sometimes hail.
The Cloud forms from UPDRAFTS of 100 MPH and when it hits the Stratsophere it flattens out to form the top of 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 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.
A cloud that indicates a storm is approaching is a cumulonimbus cloud. It is a large, dense cloud that forms due to strong upward air currents and is known for causing thunderstorms and severe weather. Cumulonimbus clouds are often characterized by their towering, anvil-shaped appearance.
A thunderstorm forms as the result of a mass of warm, moist air rising because it is more buoyant than the air around it. Eventually this mass of air reaches a layer (often the tropopause) that it cannot rise through. However, the air beneath is still rising, so the top of the air mass, and thus the top of the cloud, is forced to spread out.
It is usually just called a debris cloud or dust whirl.
A thunderstorm typically forms cumulonimbus clouds, which are tall, dense, and vertically developed clouds known for their anvil-shaped top. These clouds can bring heavy rain, lightning, thunder, and sometimes severe weather like hail or tornadoes.
stratus cloud
A cloud forms small thunder storms
The mesocyclone is typically located next to the wall cloud, in the rear portion of the thunderstorm updraft. The wall cloud is the lowering, rotating cloud that often forms at the base of a supercell thunderstorm where the mesocyclone is present.
The temperature of a body of air will typically decrease when a cloud forms. This is because the cloud forms a buffer between the air and the suns warming rays.