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Hail forms in thunderstorms (cumulonimbus clouds) when large updrafts carry water droplets high into the atmosphere where the air is much colder. The water freezes into ice and falls, only to be carried back up again by another updraft, where another layer of ice accumulates on the outside. After numerous trips, gaining more and more layers, the hailstone is too heavy to be lifted aloft by the updrafts, and falls to the ground.
Hail is mostly associated with severe thunderstorms, particularly those that produce strong updrafts and intense precipitation. It forms in cumulonimbus clouds when supercooled water droplets collide with ice particles, creating layers of ice as they are lifted and dropped within the storm. Hail is often linked to damaging weather events, including high winds and heavy rainfall. Its size and potential for destruction can vary, with larger hailstones capable of causing significant property damage and agricultural loss.
As a front continues to move, it typically leads to the formation of stratiform clouds, particularly nimbostratus clouds. These clouds develop when warm, moist air is lifted over a cold front, leading to widespread, steady precipitation. Additionally, as the front advances, it can also create cumulonimbus clouds associated with more intense weather phenomena, such as thunderstorms.
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Convection
Inside a cumulonimbus cloud, water droplets and ice particles coexist at different altitudes due to varying temperatures. As the particles collide and merge, they grow in size. Rain forms when the particles become heavy enough to fall. Hail forms when strong updrafts lift the particles back up into colder regions where they accumulate more ice layers before eventually becoming heavy enough to fall as hailstones.
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 forms within cumulonimbus clouds due to the strong updrafts that characterize these towering clouds. As water droplets are lifted into the colder upper regions of the cloud, they freeze and accumulate layers of ice. This process can repeat multiple times as the hailstones are cycled through the cloud, growing larger until they become too heavy to be supported by the updrafts and fall to the ground as hail. Thus, the presence of cumulonimbus clouds, with their intense vertical development and turbulent conditions, is crucial for hail formation.
When warm air is suddenly lifted over cold air, it cools rapidly as it rises, leading to condensation and the formation of clouds. This process can result in the development of precipitation, such as rain or snow, depending on the temperature. Additionally, the lifting of warm air can create instability in the atmosphere, potentially leading to thunderstorms or other severe weather events.
Nimbostratus is a thick cloud, typically formed on a warm front, as air is lifted over a large area (i.e. mass ascent). Precipitation is rain or snow (or a mix of both), and this can last for several hours.A cumulonimbus is formed by convection and is much taller than it is wide. Cumulonimbus clouds bring heavy showersof rain or snow, but they also bring thunder and lightning and hail. The showers will usually last for less than one hour.Finally, if you look at the bottom of a cumulonimbus cloud, you may see dark pouches (called mammatus) hanging down. These are caused by air currents trying to fall to the ground.You won't see mammatus under Nimbostratus, nor will you get thunder and lightning or hail. Thunderstorms = Cumulonimbus.
Hail forms in thunderstorms (cumulonimbus clouds) when large updrafts carry water droplets high into the atmosphere where the air is much colder. The water freezes into ice and falls, only to be carried back up again by another updraft, where another layer of ice accumulates on the outside. After numerous trips, gaining more and more layers, the hailstone is too heavy to be lifted aloft by the updrafts, and falls to the ground.
Yes, lifted is a verb.
Get Lifted was created in 2001.
A cumulonimbus cloud developed when air is lifted to a point that it is warmer, and thus less dense than its surroundings, causing it to continue to rise. Condensing water vapor prevents the rising air from cooling to quickly. The air will continue to rise until it encounters a warmer layer of air. Sometimes and inversion, somtimes it is the stratosphere. In the upper part of the cumulonimbus cloud ice crystals form. These gradually grow into snowflakes and small pellets called graupel. The snow or graupel then falls, but melts to form rain before reaching the ground The rain causes downdrafts, which produce the wind associated with thunderstorms. Finally, as ice crystals bump into each other, electrons get transferred, and different regions of the storm develop positive and negative charges. Eventually these charge differences are releases as enormous bolts of static electricity called lightning. The lightning superheats the air instantly, generating a shockwave that we hear as thunder.
Hail is mostly associated with severe thunderstorms, particularly those that produce strong updrafts and intense precipitation. It forms in cumulonimbus clouds when supercooled water droplets collide with ice particles, creating layers of ice as they are lifted and dropped within the storm. Hail is often linked to damaging weather events, including high winds and heavy rainfall. Its size and potential for destruction can vary, with larger hailstones capable of causing significant property damage and agricultural loss.
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NO, Titanic has found on September 1,1985. But it is not lifted out.