No that is false
Tornadoes are typically associated with heavy rainfall, hail, and sometimes lightning. The strong updrafts within a tornado can cause water droplets to be lifted into the cloud where they freeze and form hailstones.
Hail is formed within cumulonimbus clouds during thunderstorms when updrafts carry raindrops into extremely cold regions of the atmosphere. The raindrops freeze into ice as they are lifted higher into the cloud. This process continues as the ice particles collide with supercooled water droplets, growing larger and heavier until finally falling to the ground as hailstones once they become too heavy for the updrafts to support.
The rock will be lifted by the force f for as long as the force is applied to it.
Tornadoes lift objects through the strong upward motion of their rotating winds. As the tornado's winds spin rapidly, they create a low-pressure system that causes air and debris to be lifted off the ground. The powerful wind speeds and rotating motion of the tornado contribute to its ability to lift heavy objects and debris.
When an object is lifted 6 feet off the ground, its potential energy is a certain value based on its height and mass. If the same object is then lifted 12 feet off the ground, its potential energy will be doubled compared to when it was lifted 6 feet. This is because potential energy is directly proportional to the height to which the object is lifted.
Hailstones grow in thunderstorms through a process called accretion. As updrafts carry water droplets high into the cold upper atmosphere, these droplets freeze and form ice pellets. As the pellets are lifted and dropped multiple times within the storm, they collect additional layers of water that freeze upon contact, causing the hailstones to grow larger. Eventually, when they become too heavy for the updrafts to support, they fall to the ground as hail.
You prove that you are who you say you are, and you request that the freeze be lifted. When you established the freeze on your credit report, you were given instructions about how to 'un-freeze' it -- you can follow those instructions.
The first step in each type of precipitation begins with the condensation of water vapor in the atmosphere. In the case of rain, this condensation forms droplets that grow heavy enough to fall. For snow, the water vapor directly crystallizes into ice crystals in colder temperatures. In the case of sleet or hail, the droplets can freeze or be lifted by updrafts, respectively, before falling to the ground.
Hail forms in strong thunderstorms with intense updrafts. As water droplets are lifted high into the cloud, they freeze and collect layers of ice. When they become too heavy for the updrafts to support, they fall to the ground as hailstones. The size of the hailstones depends on the strength of the updrafts and the amount of moisture in the cloud.
Hail typically forms in strong thunderstorms where there are intense updrafts that carry water droplets upward into extremely cold areas of the atmosphere. The temperature in these upper regions can be below freezing, often around -20 to -30 degrees Celsius (-4 to -22 degrees Fahrenheit). As the droplets are lifted and fall multiple times, they freeze and accumulate layers of ice before becoming heavy enough to fall to the ground as hail.
Tornadoes are typically associated with heavy rainfall, hail, and sometimes lightning. The strong updrafts within a tornado can cause water droplets to be lifted into the cloud where they freeze and form hailstones.
Hail is most likely to form in strong thunderstorms with intense updrafts, where water droplets are carried upward into extremely cold regions of the atmosphere. These updrafts allow the droplets to freeze and accumulate layers of ice as they are repeatedly lifted and dropped. When the hailstones become too heavy for the updrafts to support, they fall to the ground as hail. Conditions such as severe thunderstorms, particularly those associated with supercells, are optimal for hail formation.
Clouds are made up of tiny water droplets or ice crystals that have condensed from moist air. These droplets are light enough to be lifted by air currents and can accumulate to form visible clouds in the atmosphere. The rising of these droplets is a result of convective processes, or warm air rising and lifting the moist air with it.
Water droplets are lifted upward in a cloud primarily by updrafts, which are currents of air that move vertically. As the air rises, it cools and expands, leading to condensation of water vapor into liquid droplets. These droplets eventually coalesce to form clouds.
Raindrops that are lifted by updrafts in thunderstorms experience rapid cooling as they ascend into colder regions of the atmosphere. When these droplets freeze, they accumulate layers of ice, resulting in the formation of hailstones. This process can repeat multiple times, causing the hailstones to grow larger before they eventually fall to the ground. The size and strength of the updrafts play a crucial role in determining the final size of the hail.
The term that describes layered and round formations of ice that form in cumulonimbus clouds is "hail." Hailstones develop through a process of updrafts and downdrafts within the cloud, allowing water droplets to freeze in layers as they are repeatedly lifted and dropped. This results in the characteristic round shape and layered structure of hail.
Hail can become baseball-sized when strong thunderstorms produce intense updrafts that carry water droplets high into the atmosphere, where temperatures are below freezing. These droplets freeze upon contact with ice nuclei and are repeatedly lifted and dropped in the storm, accumulating layers of ice. As the hailstones grow larger with each cycle, they can reach significant sizes before falling to the ground when the updrafts can no longer support their weight. This process requires specific atmospheric conditions, including strong vertical wind shear and a significant amount of moisture.