另一个低气压区正从大西洋逼近。
于是,空气总是从冷的地方流向热的地方,而风则从高气压地区吹向低气压区。
Thus, air ordinarily moves from cooler places to warmer places, and winds blow from high pressure areas to low pressure areas.
这两起事件与一种大规模的大气环流模式有关,该模式正在俄罗斯上空形成一片持续时间很久的高气压区。
The two events are linked by a large-scale pattern of atmospheric circulation which is producing a particularly persistent area of high pressure over Russia.
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