hail is your answer
Strong updrafts within a thunderhead cloud can produce severe weather phenomena such as lightning, hail, and tornadoes. These updrafts are responsible for carrying warm, moist air rapidly upward, leading to the formation of powerful storms.
Strong updrafts within a thunderhead can produce severe weather phenomena such as lightning, large hail, and heavy rain. These updrafts are responsible for the rapid vertical development of the cloud and can reach speeds of up to 100 mph.
Hailstones remain suspended in a cloud due to the strong updrafts present within the cloud. As the hailstones are being formed, they are continuously lifted higher into the colder regions of the cloud by these updrafts. This cycle repeats until the hailstones become too heavy and fall to the ground as precipitation.
A tornado is a type of severe weather phenomenon that can form within certain types of clouds, specifically supercell thunderstorm clouds. Tornadoes are associated with strong updrafts and rotating winds within these storm clouds. While not all clouds produce tornadoes, the presence of specific cloud types can contribute to the formation of tornadoes under the right atmospheric conditions.
Hail is created during severe thunderstorms when updrafts carry water droplets to the upper atmosphere where they freeze into ice. The ice pellets continue to grow as they are circulated within the storm cloud, eventually becoming heavy enough to fall to the ground as hail.
Strong updrafts within a thunderhead cloud can produce severe weather phenomena such as lightning, hail, and tornadoes. These updrafts are responsible for carrying warm, moist air rapidly upward, leading to the formation of powerful storms.
Strong updrafts within a thunderhead can produce severe weather phenomena such as lightning, large hail, and heavy rain. These updrafts are responsible for the rapid vertical development of the cloud and can reach speeds of up to 100 mph.
A cumulonimbus cloud can produce rain or hail depending on the strength of updrafts within the cloud. If the updrafts are strong enough to carry water droplets high into the cloud where they freeze, hailstones may form. If the updrafts are not as strong, the water droplets will fall as rain.
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.
Hailstones remain suspended in a cloud due to the strong updrafts present within the cloud. As the hailstones are being formed, they are continuously lifted higher into the colder regions of the cloud by these updrafts. This cycle repeats until the hailstones become too heavy and fall to the ground as precipitation.
A thunderstorm cloud is a type of rain cloud that produces thunder and lightning due to the presence of strong updrafts and downdrafts within the cloud. While rain clouds can produce precipitation in the form of rain, they do not necessarily have the same intense vertical movement and electrical activity as thunderstorm clouds.
strong updrafts of air in the cumulonimbus cloud
Clouds produce precipitation when the water droplets or ice crystals within the cloud grow to a size that they can no longer be supported by the air currents, causing them to fall to the ground. This occurs when the droplets or crystals collide and combine or when they become heavy enough to overcome the updrafts within the cloud.
A tornado is a type of severe weather phenomenon that can form within certain types of clouds, specifically supercell thunderstorm clouds. Tornadoes are associated with strong updrafts and rotating winds within these storm clouds. While not all clouds produce tornadoes, the presence of specific cloud types can contribute to the formation of tornadoes under the right atmospheric conditions.
strong updrafts of air in the cumulonimbus cloud
updrafts
Hail is created during severe thunderstorms when updrafts carry water droplets to the upper atmosphere where they freeze into ice. The ice pellets continue to grow as they are circulated within the storm cloud, eventually becoming heavy enough to fall to the ground as hail.