Tropical cyclones typically develop in late summer because that is when sea surface temperatures are at their warmest, providing the necessary fuel for the storms to form and strengthen. Warm ocean water evaporates more easily, creating the moist air needed for tropical cyclones to develop.
The Coriolis force, caused by the rotation of the Earth, is crucial in the formation of tropical cyclones. It causes air to be deflected relative to the Earth's surface, creating a spinning motion in the atmosphere that helps organize the storm. Latent heat, released when water vapor condenses into clouds and rain, provides additional energy to tropical cyclones, helping them to intensify and maintain their strength.
The stage of development of a tropical cyclone can be classified into several stages, including tropical disturbance, tropical depression, tropical storm, and hurricane. The specific stage of the tropical cyclone under research will depend on factors such as wind speed, pressure, and organization of the storm system.
Category 1 tropical cyclones can be more destructive than Category 5 storms in certain situations because they tend to be larger in size and move more slowly, resulting in prolonged periods of heavy rainfall, storm surge, and high winds. Additionally, Category 1 storms can impact areas that are not as well prepared for hurricanes, leading to more damage and disruption. On the other hand, Category 5 hurricanes have extremely high wind speeds that can cause catastrophic damage in a very short amount of time but may affect a smaller area compared to a less intense storm.
Why do tropical cyclones develop in late summer?
• What is the impact of coriolis force and latent heat on the development of tropical cyciones?
• Discuss the stage of development of the tropical cyclone under research.
• Why can category 1 tropical cyciones be more destructive (damaging) than category 5
tropical cyclones
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