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.
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.
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.
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.
Cumulonimbus clouds form when warm moist air rises rapidly, creating a tall and vertically developed cloud. Within the cloud, strong updrafts and downdrafts keep water droplets and ice particles circulating, causing them to collide and merge. In regions with strong updrafts, rain forms from the merging droplets, while hailstones can form in areas of strong updrafts where supercooled water freezes onto ice particles.
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.
Hail forms within strong thunderstorms where intense updrafts carry water droplets upward into extremely cold areas of the atmosphere. As these droplets ascend, they freeze and can accumulate layers of ice, growing larger as they are repeatedly lifted and dropped by the updrafts. The strength of the updrafts is crucial; stronger updrafts can support larger hailstones by keeping them suspended longer, allowing for more ice accumulation before they eventually fall to the ground. Thus, the relationship between hail and wind updrafts is directly tied to the updraft's strength and duration in a storm.
Moist air is lifted vertically, causing it to cool and reach its dew point. Water vapor condenses onto tiny particles in the air, forming cloud droplets. These droplets combine and grow in size until they become visible clouds.
Hail forms in strong thunderstorms with intense updrafts that carry water droplets upward into extremely cold areas of the atmosphere, where they freeze into ice. As these ice pellets are lifted and dropped repeatedly, they accumulate layers of ice until they become too heavy for the updrafts to support, causing them to fall to the ground. Hail typically occurs during severe thunderstorms, often in spring and summer when conditions are most favorable for such storms.
Different types of clouds can be involved - nimbostratus, different types of cumulus... the type of cloud isn't at all central to a blizzard. In fact, ground blizzards don't need clouds at all- much of the snow blowing around is lifted from previous falls.
Clouds are made up of tiny water droplets or ice crystals that are suspended in the air. These water droplets are so small and light that the force of air resistance keeps them lifted in the atmosphere. Gravity tries to pull the clouds down, but the upward force of air resistance helps to keep them afloat.