台风怎么形成的？

Typhoons are powerful tropical storms that form over warm ocean waters. They start as clusters of thunderstorms.

台风是强大的热带风暴，形成于温暖的海洋水域。它们起初是雷暴簇。

When the ocean surface is warm, it heats the air above, causing it to rise and create a low-pressure area. This rising air cools and forms clouds, releasing heat that fuels the storm.

当海面温度升高时，它加热上方的空气，导致空气上升并形成低压区。上升的空气冷却并形成云层，释放热量，给风暴提供能量。

As the storm grows, it begins to rotate due to the Earth's rotation, forming a cyclone. The winds spiral around the low-pressure center, and if conditions are right, the storm becomes a typhoon.

随着风暴的发展，它开始因地球自转而旋转，形成气旋。风绕着低压中心旋转，如果条件合适，风暴就会增强成台风。

Typhoons bring strong winds and heavy rain, causing significant damage when they hit land. Knowing how they form helps us prepare for these natural disasters.

台风登陆时会带来强风和暴雨，并造成重大破坏。了解它们的形成过程有助于我们为这些自然灾害做好准备。