mature stage.
The second stage during a thunderstorm is the mature stage. During this stage, updrafts continue to strengthen, causing the storm to reach its peak intensity, with heavy rainfall, strong winds, hail, lightning, and thunder.
Severe thunderstorms can reach heights up to 60,000 feet, while ordinary thunderstorms typically reach heights of around 30,000 to 40,000 feet. This difference in height is due to the stronger updrafts found in severe thunderstorms, allowing them to build higher into the atmosphere.
Cirrus clouds generally do not bring thunderstorms. They are high-level clouds composed of ice crystals and are typically associated with fair weather. Thunderstorms are usually associated with cumulonimbus clouds, which are large and dense clouds that can reach high altitudes and produce thunder, lightning, and heavy precipitation.
Thunderstorm winds rotate at varying speeds depending on the size and strength of the storm. In severe thunderstorms known as supercells, wind rotation can reach speeds of 50-60 mph (80-97 km/h) or even higher. This rotation can lead to the formation of tornadoes within the storm.
mature stage.
Thunderstorms can vary in size, but some can reach over 10 miles in diameter and extend up to 50,000 feet into the atmosphere. These large thunderstorms, known as supercells, can produce severe weather such as tornadoes, large hail, and damaging winds.
The climax of a story typically occurs near the end, when the tension and conflict reach their peak. It is the moment of greatest emotional intensity or suspense, where the outcome of the main conflict is revealed or decided.
During Darius the Great's reign at the end of the 6th Century BCE.
The greatest amount of solar energy reaches the surface of the ocean near the equator. This is because the sun's rays are more direct at the equator, resulting in higher solar intensity. Additionally, the equatorial regions generally experience less cloud cover, allowing more sunlight to reach the surface of the ocean.
No. It was under Trajan that the empire reached its largest size.
Cumulonimbus clouds typically bring thunderstorms. These are large, dense clouds that can reach high altitudes, creating an unstable atmosphere conducive to the development of thunderstorms. They are characterized by their towering, anvil-shaped appearance.
The second stage during a thunderstorm is the mature stage. During this stage, updrafts continue to strengthen, causing the storm to reach its peak intensity, with heavy rainfall, strong winds, hail, lightning, and thunder.
There were no recorded F5 tornadoes in Cleveland, Ohio from 1969 to 1972. Ohio has had tornadoes reach F5 intensity in the past, but there is no historical record of one occurring in Cleveland during that time period.
Severe thunderstorms can reach heights up to 60,000 feet, while ordinary thunderstorms typically reach heights of around 30,000 to 40,000 feet. This difference in height is due to the stronger updrafts found in severe thunderstorms, allowing them to build higher into the atmosphere.
Cirrus clouds generally do not bring thunderstorms. They are high-level clouds composed of ice crystals and are typically associated with fair weather. Thunderstorms are usually associated with cumulonimbus clouds, which are large and dense clouds that can reach high altitudes and produce thunder, lightning, and heavy precipitation.
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