The only difference between a hurricane, a cyclone, and a typhoon is the location where the storm occurs.
They all happen in the same way:
Warm water heats the air and it starts to rise, and begins to spiral. The warm air will be very moist and will start to condense. As the warm air spiral goes up into colder air, it becomes even warmer and lighter, so it rises and spirals faster, sucking in more warm moist air from the surrounding sea. This enormous heat-engine, powered by the heat in the sea, is a storm formation.
When a building stands in the path of the wind, the windward wall tends to block the air, and the air pressure increases. This force can cave in walls, smash doors or columns or bracing systems, or push buildings completely over. As it passes over, the wind can come from every direction.
If there is an opening in the windward side, the high pressure can find its way into a building. The whole building can be blown outwards, like a balloon. What makes the situation worse is that the wind is not a steady […]