America's "windbelt" runs from Texas up to the Dakotas.
美国“风带”南起德克萨斯州北至南、北达科他州。
2
The third windbelt develops as cold polar air sinks and moves south, is deflected to the right, and is therefore called the polar easterlies.
当冷的极地的空气下沉并且移动南方，受科氏力影响偏向右边，因此被称为极地东风带。
3
The reason of the strengthening of severe windbelt of low layer is due to the dynamicforce effect of upper layer jet and the transport effect of air particle of low latitude.